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32E12SW00H 63.5467 NOSEWORTHY 010<br />

COGEMA CANADA LIMITED<br />

DETAILED MAPPING and<br />

LITHOGEOCHEMISTRY RESULTS<br />

- TRENCH #5 -<br />

1 ll<br />

Ref. No. 87-CND-47-06<br />

(Document #0076U)<br />

By: A. Morin<br />

November 1987


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SUMMARY OF RESULTS<br />

1. INTRODUCTION<br />

2. LITHOLOGY<br />

32E12SW08M 63.5467 NOSEWORTHY<br />

TABLE OF CONTENTS<br />

Rhyolite l felsic tuff ......... . .. .. ....... .. .... l<br />

Iron-rich tuff and dacitic tuff .................. 3<br />

Iron-rich tuff of southern section .. . .. ..... .. . .. 4<br />

Dacitic ashfall tuff of southern section .. ...... . 4<br />

Rock alteration .................................. 4<br />

3. LATE DYKE AND VEINING<br />

4. STRUCTURE<br />

Diabase dyke ................................,. ... 5<br />

Quartz veining ... . . .. .. .. . . . . . . . . .. .. . .. . . .. . .. . . 5<br />

5. LATE FRACTURES<br />

6. GLACIAL STRIAE<br />

REFERENCE . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .<br />

Figure l :<br />

Figure 2 :<br />

Figure 3 :<br />

LIST OF FIGURES<br />

Location of camps and work sites, fall 1986 outcrop<br />

stripping program. Scale 1:50 000 .. .. .... . .. . .. . ...<br />

Histogram of late fracture orientations from<br />

trench 5 (azimuth only).<br />

Total number of observations is 113 .. .. ... .. . . . . . ..<br />

Histogram of glacial striae directions measured at<br />

trench 5 and compiled for all trenches. Total number<br />

of measures is 35 at trench 5 and 78 for trenches<br />

l through 5 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ...<br />

page<br />

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O10C


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SUMMARY OF RESULTS<br />

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Four different rock types are exposed at Trench 5. To the north, the rock<br />

consists of a massive to locally weakly foliated rhyolite or acid tuff. The<br />

central and southern part of the northern section is covered by an interbedding<br />

of iron-rich garnetiferous lapilli tuff to agglomerate and dacitic,<br />

locally garnetiferous ashfall tuff to agglomerate. The two small outcrops of<br />

the southern section consist of a dark green iron-rich tuff (locally with<br />

clasts) and of dacitic ashfall tuff. A diabase dyke, trending north-south, is<br />

exposed on the east margin of the outcrops.<br />

The rocks are generally steeply north dipping with a strike ENE-WSW.<br />

Minor folds are common, the fold axes plunge gently to the east. Quartz<br />

veinings can be locally abundant with/without epidote. Generally quartz veins<br />

are slightly discordant compared to the foliation (angle between vein and<br />

foliation varies from 10 0 to 20 0 ).<br />

Sixteen samples were taken for chemistry and/or thin section. Nine<br />

samples are below the detection limit for Au (2 ppb). Five samples are<br />

between 4 and 11 ppb. One sample gives 110 ppb, it came from a locally<br />

strongly pyritiferous ashfall tuff. No whole rock analysis was done.


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l. INTRODUCTION<br />

Trench 5 consists of two parts, a northern part (outcrop GC-1) and a<br />

southern part (outcrop GC-2), ninety metres separate these two outcrops.<br />

This trench is located 350 metres north of the southern limit of the<br />

property and approximately 1.3 kilometres east of the Burntbush River<br />

(see Fig. 1).<br />

This trench was mechanically stripped and cleaned during the 1986 fall<br />

program. Approximately 4400 metres^ were cleared of trees and 2500<br />

metres^ of bedrock were exposed. Mapping was not performed at that time<br />

due to poor weather conditions. Work started again in July 1987 with the<br />

completion of the 5x5 metres grid and mapping of the outcrop.<br />

In order to make the description easier, the different lithologies<br />

encountered will be discussed from north to south.<br />

2. LITHOLOGY<br />

Rhyolite / felsic tuff<br />

This rock type consists of a very fine to fine grained, non-magnetic,<br />

massive to weakly foliated rhyolite flow or acid tuff. Colour varies<br />

from greenish to brownish to buff and white (the rock is white when<br />

there is no veining in the area) on the weathered surface; and bluish<br />

grey on the fresh surface.<br />

In general, the rock has a massive aspect, but usually a weak<br />

foliation or banding is observed in hand specimen. The foliation<br />

orientation is quite variable but usually the dip is shallow,<br />

measurements are very difficult to take. The foliation is better<br />

developed near the quartz veins (might be related to the formation of<br />

veins) and close to the contact between this unit and the iron-rich<br />

tuff. Foliation measurements taken close to the contact have more or<br />

less the same orientation as the contact with a strong dip to the<br />

north. One possible explanation for the absence of foliation on the<br />

outcrop surface is that the foliation plane is parallel to the<br />

surface.<br />

The presence in two areas of a dark green massive facies which might<br />

represent the undeformed equivalent of the well foliated iron-rich<br />

tuff was noted. This, the rhyolite/acid tuff, might correspond to<br />

the dacitic tuff.<br />

- l -


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Figure l : Location of camps and work sites, fall 1986<br />

outcrop stripping program.<br />

Scale 1:50 000<br />

- 2


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One thin section taken in 1986 from this unit gave 757. plagioclase,<br />

57. quartz and zoisite and 107. opaques.<br />

The contact between this unit and the iron-rich tuff is sharp and<br />

runs more or less N100 0 . It is very easy to follow, mostly because<br />

of the colour change and of a well defined foliation in the iron-rich<br />

tuff. The contact seems faulted. Foliations on both sides of the<br />

contact follow the direction of the contact.<br />

Iron-rich tuff and dacitic tuff<br />

These two rock types will be discussed together because in outcrop,<br />

they are often interbedded or closely related. Three sub-units were<br />

mapped based on the relative abundance of each unit: iron-rich tuff<br />

(lapilli to agglomerate), dacitic tuff (lapilli to agglomerate) or<br />

mixed tuff where there is a rapid interbedding of the two facies or<br />

where the rock seems to be a transition facies (especially on top of<br />

outcrop where the rock was originally exposed and covered by lichen:<br />

the composition seems to be intermediate between the two.<br />

The iron-rich tuff is medium green on the weathered surface and dark<br />

greenish grey on fresh surface. Usually the rock is fine grained and<br />

well foliated with coarse grained almandine garnets. Garnets are<br />

almost everywhere, they have no specific orientation. On the<br />

weathered surface, this unit is spotted with small elongated rusty<br />

nodules (mm to cm size) with no associated magnetism (altered<br />

magnetite crystals). This unit is generally very rich in clasts of<br />

two types: one type of clast is biotite-rich brownish and it is<br />

weathering in comparison with tuff; the other type is whitish and<br />

does not weather in. The clasts are garnet and magnetite free. The<br />

clasts are flattened and elongated in the direction of foliation.<br />

The ratio length to width varies from 2:1 to more than 10:1. Looking<br />

at the clast distribution, one can deduce that the foliation is<br />

parallel to the bedding.<br />

The iron-rich tuff is relatively more abundant than the dacitic tuff<br />

on the map. But the true importance of each unit is unknown. On a<br />

vertical face, the iron-rich tuff was overlain by dacitic tuff.<br />

The dacitic tuff weathers light brown to buff and it is dark grey on<br />

fresh surface. The grain size is again fine to very fine with<br />

feldspar phenocrysts, the foliation is generally well developed.<br />

This tuff carries less clasts (same types as in iron-rich).<br />

Almandine garnets are locally observed but in lesser amount than in<br />

the iron-rich tuff. No rusty nodules are observed. Two thin<br />

sections were taken in this unit and have a very similar mineralogy -<br />

plagio- clase-quartz-epidote-lepidomelane-chlorite and opaque. The<br />

texture observed in the slide is mylonitic to blastomylonitic.<br />

- 3 -


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Iron-rich tuff of southern section<br />

This outcrop is dark green tp olive green on the weathered surface<br />

and dark greenish grey on the fresh surface. The foliation/<br />

schistosity is very well developed. This unit is very similar to the<br />

iron-rich tuff of the northern section but with some minor<br />

differences. The clasts are less abundant, they are observed in the<br />

eastern part of the outcrop. There is only one type of clast, white<br />

on weathered surface, massive looking. Here again the clasts are<br />

elongated and flattened. The foliation may be different from the<br />

bedding (using the clast distribution). Garnets are scarce, they are<br />

observed in 2 distinct areas. There is no interbedding with the<br />

dacitic tuff. Millimetric to centimetric elongated rusty nodules<br />

are present everywhere on the outcrop. According to a thin section<br />

taken in 1986, quartz and feldspar are the main constituents with<br />

biotite, chlorite and calcite, the texture is mylonitic.<br />

The southernmost part of this outcrop has a different aspect; it<br />

looks like a transition facies between this unit and the dacitic unit<br />

exposed to the south. The strong glacial polish makes the<br />

interpretation more difficult because it tends to obliterate textures<br />

and relations.<br />

Dacitic ashfall tuff of southern section<br />

This dacitic ashfall tuff with feldspar phenocrysts is well foliated<br />

and is clast and garnet free and with a meter thick layer parallel to<br />

the foliation of a more massive buff coloured rock (reminiscent of<br />

the rhyolite/acid tuff of the northern section). No thin section was<br />

taken from this outcrop. Close to the iron-rich tuff there is again<br />

a transition facies but with a well developed glacial polish; the<br />

identification is very difficult.<br />

Rock alteration<br />

There is no major rock alteration in trench 5. The entire outcrop<br />

looks relatively fresh. Nevertheless there are some interesting<br />

points.<br />

A local silicification is observed close to a sheared, pyrite-rich<br />

section of the lapilli tuff/agglomerate (sample T-5-1 was taken in<br />

this area and yields 110 ppb Au). Close to some quartz-epidote veins<br />

or patches, there is a minor epidotization of the host rock. There<br />

is also the transformation of iron oxides (magnetite) into rusty/<br />

limonite nodules on the weathered surface of the outcrop.


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3. LATE DYKE AND VEINING<br />

Diabase dyke<br />

A diabase dyke crosscuts the east part of the northern and southern<br />

sections of trench 5. The intrusive contact with the host rock is<br />

well exposed. The host rock did not undergo any major transformation<br />

(none observed at the macroscopic scale). There is a chill zone in<br />

the diabase with a thickness of less than fifteen centimetres. The<br />

true thickness of the dyke is unknown but it exceeds twenty five<br />

metres.<br />

The dyke is strongly magnetic, massive looking and medium to coarse<br />

grained. Rare quartz veins and fractures crosscut the diabase but<br />

stop before reaching the host rock. In places there are inclusions<br />

of host rock fragments (approximately 50 centimetres long).<br />

Some centimetric to decimetric offshots of diabase are found in the<br />

host rock. The diabase found in the westernmost part of the southern<br />

section is probably part of the ramification system.<br />

Quartz veining<br />

Quartz veins are not evenly distributed over the entire trench.<br />

There are areas where veining is very important and areas where<br />

veining is practically absent. For the mapping purpose, small quartz<br />

veins were not drawn.<br />

Three major types of quartz veins are seen on the outcrop: quartzepidote<br />

± chlorite (chlorite may replace partially or completely<br />

epidote) or quartz alone; quartz-tourmaline veins are observed only<br />

in the iron-rich tuff of the southern section. Veins can be<br />

undeformed, folded or boudinaged. There are also at least two<br />

generations of veining and at least one older than the intrusion of<br />

the diabase dyke.<br />

In the quartz epidote veins, quartz is in the center while epidote is<br />

forming the external envelope. In places, epidote extends in the<br />

host rock. Epidote alone can form small isolated veins, but this is<br />

a very minor type.<br />

The general orientation of veins is East-West with a strong dip. In<br />

the northern section, veins are more or less concordant with the<br />

foliation whereas in the southern section, veins are making an angle<br />

of 10 to 20 degrees with the foliation (i.e. foliation at N80 0 , veins<br />

- 5 -


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4. STRUCTURE<br />

are between 90" and 100 0 ). The vein thickness is usually less than<br />

thirty centimetres but veins with an observed thickness of one metre<br />

or more are described. Veins can be sterile or weakly mineralized<br />

(sulphides).<br />

Foliation near the quartz segregations is very strongly disturbed and<br />

folded (centimetric/decimetric folding).<br />

The intensity of deformation is variable from one end of trench 5 to the<br />

other end. Rhyolite/acid tuff of the northern section is undeformed. The<br />

only deformation observed in this area is located near the contact with<br />

the adjacent unit where there is a development of foliation parallel to<br />

the contact.<br />

Deformation in the iron-rich and dacitic tuffs is also quite variable.<br />

The deformation is stronger than in the rhyolite/acid tuff. The degree of<br />

deformation can be visualized by the flattening and elongation of the<br />

clasts within the tuff (ratio length: width varying from 2:1 to 10:1). In<br />

thin section, the texture is mylonitic to blastomylonite (GC-02-04).<br />

Shearing observed in trench 5 is at a local (minor) scale, not comparable<br />

with the shearing observed at trench #2 (report 87-CND-47-01). The<br />

iron-rich tuff of the southern section shows the maximal shearing observed.<br />

Shearing increases towards in most cases, in the iron-rich and dacitic<br />

tuffs, foliation varies between N75 0 and N85 0 and it is steeply<br />

north-dipping (65 0 -85 0 ). In rare cases, foliation is vertical or steeply<br />

south dipping.<br />

Microfoldings observed in dacitic and iron-rich units (mostly associated<br />

with quartz veining) are similar or comparable to those observed in Trench<br />

3 with an easterly direction of fold axes and a plunge of 25 0 or less. No<br />

stereographic projection of foliation or fold axes was done because of<br />

similarity with trench 3. Few lineations (folds lineation) were developed<br />

but no measurement was taken.<br />

5. LATE FRACTURES<br />

Fractures are oriented in all directions usually with a steep dip (most<br />

time not measurable). 161 of all fractures are between NlO 0 and N55 0 ; 237o<br />

are between 65 0 and 100 0 , and 607o of all fractures are between 100 0 and<br />

ISO 0 (see Fig. 2). Some minor displacements are observed in places (OO<br />

cm). Most fractures are bleached, the bleaching envelope is narrow.<br />

- 6 -


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g22S22S8g ooog ggg<br />

AZIMUTH OF LATE FRACTURE<br />

Figure 2 :<br />

Histogram of late fracture orientations from<br />

trench 5 (azimuth only). Total number of<br />

observations is 113.


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Fracturing seems more abundant in the rhyolite/acid tuff than everywhere<br />

else. This impression may be caused by the absence of a well developed<br />

foliation. Fracturation in this unit forms long linear pattern.<br />

Fracturation in the iron-rich and dacitic tuffs is less obvious but here<br />

again, the pattern is the same.<br />

In the iron-rich tuff of the southern section, fracturation is different.<br />

Instead of a long linear pattern, fractures are 10 centimetres long and<br />

they are evenly spaced and oriented over a major part of the outcrop. The<br />

strike varies from N05 0 -N40 0 , dip is vertical. Most fractures are open, a<br />

few are healed with quartz.<br />

6. GLACIAL STRIAE<br />

Thirty-five (35) measures of ice direction were taken in trench 5 ranging<br />

from N125 0 to N195 0 with a maximum at N140 0 for the first set. The<br />

southeast ice direction was determined in one place by a rat tail<br />

feature. Another set (from an older glaciation) of three measures ranges<br />

from N245 0 to N255 0 (the southwest direction is inferred from regional<br />

knowledge) (see Fig. 3).<br />

Glacial polish is well developed in low areas of outcrop especially in the<br />

southern part of the northern section (outcrop GC-01) and in the southern<br />

part of the southern section (outcrop GC-02).<br />

- 8 -


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28-<br />

26-<br />

24-<br />

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0 12-<br />

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2 8.<br />

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Fi&ure 3 :<br />

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AZIMUTH OF GLACIAL STRIA<br />

•———— TRENCH 5<br />

,,.W:.:.:.x.:<br />

ALL TRENCHES<br />

li l . . ,l<br />

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O 01<br />

o<br />

Histogram of glacial striae directions measured<br />

at trench 5 and compiled for all trenches. Total<br />

number of measures is 35 at trench 5 and 78 for<br />

trenches l through 5.<br />

- 9 -<br />

8<br />

M


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REFERENCE<br />

LEARN, John, 1986, Geological Mapping and Lithogeochemistry Results,<br />

Summer Field Program, Part II (Cogema Report No. 86-CND-47-02) .<br />

1986 Detailed Mapping and Lithogeochemistry Results of Outcrop<br />

Stripping Program (Cogema Report No. 87-CND-47-01) .<br />

- 10 -


l<br />

1<br />

SAMPLE STATISTICS TRENCH 5<br />

1<br />

1<br />

Roch type and sample<br />

numbers<br />

Dacitic and iron-rich tuffs<br />

Chemistry *<br />

Opt. A Opt. B<br />

Thin section<br />

1<br />

1<br />

1<br />

GC-002<br />

GC-003<br />

GC-004<br />

GC-006<br />

GC-008<br />

GC-011<br />

T5-1 (pyrite)<br />

T5-3<br />

AM-16-4<br />

X<br />

X<br />

xxx<br />

x x<br />

x<br />

X<br />

X<br />

x<br />

x<br />

X (2)<br />

1<br />

1<br />

1<br />

1<br />

1<br />

Rhyolite/Acid Tuff<br />

AM-16-1<br />

AM-16-2<br />

AM-16-3<br />

Diabase dyke<br />

GC-001<br />

Late veins<br />

GC-005 (much host rock)<br />

GC-007 (with host rock)<br />

T5-2<br />

T5-4 (much host rock)<br />

x<br />

x x<br />

X<br />

x<br />

1<br />

TOTALS;<br />

Opt. A<br />

Opt. B<br />

Thin section<br />

1<br />

Summer program 1986<br />

Fall program 1986<br />

Summer program 1987<br />

8 0<br />

3 0<br />

4 0<br />

4<br />

4<br />

0<br />

1<br />

15 0<br />

8<br />

1<br />

1<br />

1<br />

Opt, A = minor elements,<br />

Opt. B = major and minor<br />

CaO, K20, C02<br />

elements<br />

- 11 -


l of BURNT BUSH MINOR ELEMENTS >> TRENCH [87/11/26]<br />

rd Station Sample no Au ppi Sb ppa As ppi 8a p pu Cd pp* Cs ppa Cr ppa Eu ppn Hf ppa La ppn Ho ppn Ni ppn Rb ppg Se ppm<br />

10<br />

li<br />

12<br />

S3<br />

14<br />

15<br />

16<br />

18<br />

le<br />

19<br />

20<br />

58<br />

59<br />

60<br />

61<br />

6C-2<br />

6C-3<br />

6C-4<br />

GC- 5<br />

GC-6<br />

6C-7<br />

GC-8<br />

6C-11<br />

T5-1<br />

T5-2<br />

T5-4<br />

AH-16-1<br />

Ah-16-2<br />

AM-16-3<br />

AM-16-4<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

11<br />

7<br />

-2<br />

-2<br />

4<br />

-2<br />

-2<br />

-2<br />

110<br />

-2<br />

10<br />

-2<br />

6<br />

-2<br />

-2<br />

-0.1<br />

0.1<br />

0.1<br />

0.2<br />

-0.1<br />

0.3<br />

-0.1<br />

0.3<br />

0.2<br />

0.4<br />

0.2<br />

0.1<br />

0.2<br />

0.1<br />

-0.1<br />

1<br />

1<br />

1<br />

-1<br />

-1<br />

2<br />

1<br />

-1<br />

7<br />

3<br />

4<br />

-1<br />

-1<br />

-1<br />

1<br />

390<br />

220<br />

390<br />

150<br />

150<br />

91<br />

250<br />

75<br />

260<br />

-50<br />

130<br />

560<br />

-50<br />

230<br />

380<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

-5<br />

1<br />

1<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

1<br />

0<br />

11<br />

-1<br />

2<br />

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-20<br />

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23<br />

28<br />

40<br />

35<br />

25<br />

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32<br />

100<br />

110<br />

83<br />

120<br />

14<br />

10<br />

14<br />

8<br />

14<br />

32<br />

16<br />

15<br />

18<br />

11<br />

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22<br />

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14<br />

13<br />

30<br />

28<br />

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1<br />

-1<br />

1<br />

1<br />

1<br />

-1<br />

-1<br />

1<br />

1<br />

-1<br />

1<br />

-1<br />

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3<br />

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3.5<br />

5.2<br />

5.1<br />

3.0<br />

8.1<br />

8.3<br />

3.5<br />

6.6<br />

12.0<br />

8.3<br />

12.0<br />

2.3<br />

8.8<br />

10.0<br />

2.2<br />

15<br />

9<br />

15<br />

13<br />

13<br />

15<br />

10<br />

18<br />

13<br />

12<br />

14<br />

19<br />

25<br />

18<br />

10<br />

-1<br />

-1<br />

-1<br />

-1<br />

-1<br />

-1<br />

-1<br />

-1<br />

-1<br />

1<br />

-1<br />

2<br />

-1<br />

-1<br />

1<br />

-20<br />

-20<br />

-20<br />

-20<br />

-20<br />

23<br />

24<br />

24<br />

29<br />

-20<br />

-20<br />

-20<br />

-20<br />

-20<br />

-20<br />

32<br />

25<br />

26<br />

15<br />

30<br />

-5<br />

21<br />

-6<br />

21<br />

-5<br />

14<br />

49<br />

-14<br />

30<br />

64<br />

10.0<br />

8.9<br />

13.0<br />

13.0<br />

14.0<br />

16.0<br />

14.0<br />

15.0<br />

14.0<br />

8.0<br />

14.0<br />

16.0<br />

25.5<br />

20.1<br />

16.0


l of BURNT BUSH MINOR ELEMENTS >> TRENCH #5


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COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

HAND SPECIMEN DESCRIPTION Sample No.; AM-16-1<br />

1. Mineralogy; 7o, habit, grain size: ______________________________<br />

____Too fine grained for mineral identification.__________________<br />

____Small epidote nodules observed.———^^^^——————————————-———<br />

2. Rock Texture. Colour, Hardness, etc.; ___________________._________<br />

____Light buff coloured on weathered surface, medium grey on fresh surface.<br />

3. Structures: _______<br />

————Weakly foliated<br />

. Alterations: ___________<br />

____Normal rock weathering<br />

5. Magnetism: ______<br />

————Non magnetic<br />

I^=^===^=<br />

6. Rock name (Field Designation); Rhyolite or acid tuff<br />

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(Doc. #0076U - 15.12.87)


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COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

HAND SPECIMEN DESCRIPTION Sample No.; AM-16-2<br />

1. Mineralogy: 7o. habit, grain size; ______________________________<br />

____Very fine grained.—-..,——————,———.—-—,—^^^^—^————,——.—.——,<br />

No mineral identified.___________________________________<br />

2. Rock Texture, Colour. Hardness, etc.; _______________________________<br />

————Buff coloured on weathered surface; medium greenish grey on fresh surface.<br />

————Not very hard, can be scratched by a knife.———————————^^——^^—-——<br />

____Massive to very weakly foliated.______________________________<br />

3. Structures: ,————<br />

None observed.<br />

. Alterations: __________________<br />

____Normal weathering of the rock.<br />

5. Magnetism; _____<br />

____Non magnetic<br />

6. Rock name (Field Designation): Massive rhyolite or acid tuff<br />

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(Doc. #0076U - 15.12.87)<br />

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COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

HAND SPECIMEN DESCRIPTION Sample No.; AM-16-3<br />

1. Mineralogy: f,, habit, grain size:<br />

____Very fine grained.________________________________________<br />

____Difficult to guess the mineralogy because of grain size but chlorite<br />

____or sericite is present.__________________________________<br />

____No sulphides.__________________________________________<br />

2. Rock Texture. Colour. Hardness, etc.: ____________________________<br />

____Dark green to green olive on weathered surface, dark greenish grey on<br />

____fresh surface.________________________________________<br />

____Well foliated to schistose._______________________________<br />

____Not very hard, can be scratched by a knife.-^^———^^^—————————<br />

3. Structures: ____________<br />

____Microfolding observed.<br />

. Alterations: __________________________<br />

____Rusty alteration on the weathered surface.<br />

5. Magnetism: ______<br />

____Non magnetic.<br />

zzziizziziizizz:<br />

8 6. Rock name (Field Designation); Iron-rich tuff<br />

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(Doc. #0076U - 15.12.87)


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COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

HAND SPECIMEN DESCRIPTION Sample No.; AM-16-4<br />

1. Mineralogy: 7o. habit, grain size; —————-^—————-^—^—-——————————<br />

It is too fine grained for mineral identification.______________<br />

2. Rock Texture, Colour, Hardness, etc.; _________________________<br />

____Liftht buff coloured on the weathered surface, medium greenish grey on<br />

____fresh surface.________________________________________<br />

____Fairly well foliated.____________________________________<br />

3. Structures: ————-——.——-———————.—.——.<br />

Microfolding observed in hand specimen.<br />

A, Alterations: ______<br />

____Rusty surfaces.<br />

5. Magnetism: _____<br />

____Non magnetic<br />

^^nz^iziiiizz:<br />

l 6. Rock name (Field Designation): Rhyolite X acid tuff<br />

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(Doc. #0076U - 15.12.87)


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Ref. No. 87-CND-47-04<br />

(Doc. //0076U)<br />

COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

3aE12SW0014 63.5467 NOSEWORTHY<br />

FINAL REPORT - 1987<br />

"REVERSE CIRCULATION DRILLING"<br />

VOLUME l of 3<br />

jy: j. Learn<br />

January 1988<br />

020


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TABLE OF CONTENTS<br />

32E12SW80M 63.5467 NOSEWORTHY<br />

1. INTRODUCTION.................................................. l<br />

1.1 Summary of Work Performed to date on the<br />

Burntbush River Project ............................ l<br />

1.2 Location and Access . .... .. ......................... 2<br />

1.3 Technical Summary . .. .. ...... .... ..... ........ . ..... 2<br />

1.4 Generalized Quaternary Stratigraphy of Northeastern<br />

<strong>Ontario</strong> .. . . . .. . . . .. . . . . .. ... . .... .... ....... .. ... .. 4<br />

1.5 Bedrock <strong>Geology</strong> of the Burntbush River<br />

Proj ect Area ....................................... 6<br />

2. DESCRIPTION OF FIELD WORK . . . . . . .. . . . . . . . . . . . . . . . . . . . . .. . .. . . . . 8<br />

2.1 Field Procedures ................... .. .. ............ 8<br />

2.2 Drilling and Sample Statistics ..................... 13<br />

3. OVERBURDEN RESULTS . . . . . . . . . . . . . . . . . .. . ... . . ..... .... .. . .. . .... 16<br />

3.1 Presentation of Drill Hole Sections ..... ........... 16<br />

3.2 Sample Results ...... ............................... 19<br />

3.3 Discussion of Background and Threshold Values ...... 33<br />

3.4 Interpretation of Overburden Results ............... 34<br />

4. BEDROCK GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40<br />

4.1 Introduction .........,............................. 40<br />

4.2 Metasedimentary Rocks ..... .. ......,.... ............ 40<br />

4.3 Metagabbros and Mafic to Intermediate Metavolcanics. 41<br />

4.4 Felsic to Intermediate Metavolcanic Rocks .......... 46<br />

4.5 General Summary of Bedrock Chip Studies ............ 48<br />

4.6 New Outcrop . . .......... .... .... . ..,. .. . . .. ,...... .. 49<br />

5. CONCLUSIONS................................................... 50<br />

5.1 Overburden Stratigraphy ............................ 50<br />

5.2 Overburden Sampling .. .... .. .. ........ .............. 51<br />

5.3 Bedrock <strong>Geology</strong> .................................... 51<br />

6. REFERENCE LIST ............................. . . .. . . . . . .. . ...... . 53<br />

page<br />

020C


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9<br />

LIST OF FIGURES<br />

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Figure 1-1<br />

Location of the Burntbush River Property,<br />

Northeastern <strong>Ontario</strong><br />

Figure 3-1<br />

Overburden Thicknesses on the Burntbush River<br />

Property.<br />

17<br />

Figure 3-2<br />

Drill Section L-L'<br />

19<br />

Figure 3-3<br />

Total Gold Grain Counts for Overburden Drill Holes<br />

22<br />

Figure 3-4<br />

Comparative Histograms of Gold Grain Volumes<br />

reported by ODM from the Winter and Summer<br />

Programs<br />

Figure 3-5<br />

Effects of Glacial Transport on Gold Particle<br />

Size and Shape<br />

25<br />

Figure 3-6<br />

Distribution of Irregular and Delicate Gold<br />

Grains.<br />

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LIST OF TABLES<br />

Table 1-1 : Generalized Quaternary Stratigraphy<br />

Northeastern <strong>Ontario</strong> ...................,............ 5<br />

Table 2-1 : Drilling Statistics ................................ . 14<br />

Table 2-2 : Sample Statistics ... ................................ 15<br />

Table 3-1 : Gold Grain Counts - A Summary .....................,. 21<br />

Table 3-2 : Summary of the other elements analyzed for in<br />

Heavy Mineral Concentrates ..,....................... 28<br />

Table 3-3 : As Results from Heavy Mineral Concentrates from<br />

two Tills in Holes BOB-01 and BOB-02 ................ 32<br />

Table 4-1 : Metasedimentary Rocks -<br />

Summary of Analytical Results ....................... 42<br />

Table 4-2 : Metagabbros - Summary of Analytical Results ......... 44<br />

Table 4-3 : Mafic to Intermediate Metavolcanic Rocks -<br />

Summary of Analytical Results ....................... 45<br />

Table 4-4 : Felsic to Intermediate Metavolcanic Rocks -<br />

Summary of Analytical Results ....................... 47<br />

page


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LIST OF MAPS<br />

Map l : Drill Hole Location Map. Scale 1:20 000<br />

l Maps 2 to 9 : Drill Hole Sections. Horizontal Scale 1:5000,<br />

Vertical scale 1:500<br />

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Map 10 : Bedrock <strong>Geology</strong>. Scale 1:20 000<br />

VOLUME 2 of 3:<br />

LIST OF APPENDICES<br />

Appendix I : Drilling Summary and Field Logging Sheets<br />

VOLUME 3 of 3:<br />

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— Appendix II : ODM Overburden Sample Treatment and Results<br />

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Appendix III :<br />

Chimitec HMC Sample Treatment and Results<br />

Appendix IV : Bedrock Chip Descriptions and Chemistry Results


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1. INTRODUCTION<br />

1.l Summary of Work Performed to date on the Burntbush River Project<br />

The Burntbush River project is a joint venture gold exploration<br />

program between COGBMA Canada Ltd and AMERITEX Resources Ltd. The<br />

property comprises 312 contiguous mining claims situated in<br />

northeastern <strong>Ontario</strong>.<br />

Most of the project area (300 claims) was staked for AMERITEX in<br />

January, 1984. The only work performed by them on the claims was an<br />

airborne VLF-EM and magnetics survey, which was contracted to Aerodat<br />

Ltd (Ameritex, 1984).<br />

In May 1986, COGEMA and AMERITEX signed a joint venture agreement<br />

naming COGEMA operator of the exploration program and all subsequent<br />

work has been performed by ourselves. At this time, a block of 12<br />

claims (previously held by DOME EXPLORATIONS Ltd) was added to the<br />

property.<br />

The first field program was performed in the summer of 1986, and<br />

comprised geologic traverses aimed at locating, mapping and sampling<br />

outcrops. Traverse spacing ranged from 50 to 100 m and numerous<br />

undocumented outcrops were found and described (COGEMA Ref. No.<br />

86-CND-47-02).<br />

Later, in the fall of 1986, five of the larger outcrops were stripped<br />

and detailed mapping was performed in order to better understand the<br />

geology. These outcrops are fairly well distributed across the<br />

property and represent an important step in understanding the<br />

property geology at a broader scale (COGEMA Ref. No. 87-CND-47-01).<br />

Finally, in December 1986, a second airborne survey was commissioned,<br />

this time to DIGHEM Surveys Ltd, mostly because the previous airborne<br />

survey did not include low frequency or time domain EM<br />

instrumentation (COGEMA Ref. No. 87-CND-47-02).<br />

The winter 1987 program represents the next step in our evaluation of<br />

the project area. This program consisted of reverse circulation<br />

(overburden) drilling at ~400 m x 400 m spacing and was planned to<br />

cover the southern ~ one third of the property. Unfortunately, 23<br />

of the planned drill holes could not be completed due to mild weather<br />

which made it necessary to abandon work on the east side of the<br />

Burntbush River.<br />

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Reverse circulation drilling was therefore resumed during the summer<br />

1987 program. This program was designed to complete the<br />

reconnaissance holes not yet drilled, and also to perform some<br />

detailed follow-up drilling (~200 m x 200 m spacing) in areas of<br />

interest interpreted from the results of the winter program. Results<br />

of the two programs are combined in this report.<br />

1.2 Location and Access<br />

The Burntbush River property covers about 50 km^ in the townships<br />

of Hoblitzell and Noseworthy, northeastern <strong>Ontario</strong> (see Fig. 1-1).<br />

During the winter program, access to the area was by winter road via<br />

Tomlinson Road, which connects to a main east-west maintained gravel<br />

road connecting La Sarre, Que. and Iroquois Falls, Ont.<br />

During the summer program, helicopter support from La Sarre, Que. and<br />

Cochrane, Ont. was used, but the drill itself was driven along the<br />

winter road to the property.<br />

1.3. Technical Summary<br />

Reverse circulation drilling is a commonly used technique in gold<br />

exploration in Canada, particularly where outcrop exposure is poor<br />

and where glacial overburden deposits are thick. The method is<br />

relatively well known and various aspects are described in Averill<br />

and Thomson (1981), and in Shelp (1985), and for this reason no<br />

detailed technical description will be given.<br />

Any such program is generally designed to test for 1) gold (or other)<br />

anomalies in glacial sediments (usually till) which represent<br />

mechanical dispersion trains that can hopefully be traced back to<br />

their source, and 2) bedrock mineralization.<br />

The results are therefore presented separately in two main parts: the<br />

first part (section 3) covers the Quaternary aspect of the program,<br />

and the second part (section 4) covers the bedrock geology aspect of<br />

the program.<br />

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FJRure 1-1 :<br />

Location of the Burntbush River Property,<br />

Northeastern <strong>Ontario</strong>.<br />

Scale 1:250 000<br />

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The drilling contract was awarded to HEATH and SHERWOOD Drilling Ltd<br />

who used a Nodwell mounted Acker drill, as well as a GT1000 tracked<br />

vehicle to supply water. Road clearing was performed by NORTHLAND<br />

Explorations Ltd using TD-15 (narrow track) and D-6-LGP (wide track)<br />

bulldozers.<br />

Drilling was performed between March 3 and April 4, 1987 and again<br />

between June 20 and July 7, 1987. All road construction was<br />

performed between February 17 and March 28, 1987. Note also that a<br />

total of 25.7 km of line was cut between Feb. 25 and March 14, 1987<br />

so that drill hole locations could be precisely measured.<br />

1.4. Generalized Quaternary Stratigraphy of Northeastern <strong>Ontario</strong><br />

The Abitibi region of northeastern <strong>Ontario</strong> and northwestern Quebec is<br />

overlain by a fairly complex Quaternary stratigraphy. Some published<br />

information is available (eg Boissoneau 1965, Clark and Steam 1968,<br />

Bouchard 1986), but there is no comprehensive detailed summary. Much<br />

of the information presented below has been furnished by OVERBURDEN<br />

DRILLING MANAGEMENT Ltd (ODM), who,were contracted to train us in the<br />

recognition and sampling of the various Quaternary units using the<br />

reverse circulation method.<br />

During the Pleistocene in continental North America, four major<br />

periods of glaciation are recognized. Very little evidence of the<br />

first two glaciations has been documented in the Abitibi region. The<br />

two major glaciations of importance are the Illinoian advance<br />

O125 000 years ago) and the Wisconsinan advance (from ~100 000<br />

to ~10 000 years ago).<br />

A generalized stratigraphic section is presented in Table 1-1.<br />

The Lower Till was deposited in Illinoian time and is generally<br />

preserved only in deep bedrock valleys; in most other cases it has<br />

been reworked by the more recent Wisconsinan advance.<br />

The Matheson Till was deposited in Wisconsinan time and is the major<br />

widespread till sheet in the western Abitibi region. In the northern<br />

part, a minor re-advance in late Wisconsinan time deposited the<br />

Cochrane Till.<br />

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Table 1-1 : GENERALIZED QUATERNARY STRATIGRAPHY<br />

OF NORTHEASTERN ONTARIO<br />

COCHRANE TILL (CT) (very late Wisconsinan)<br />

Cochrane Till has mostly reworked clays<br />

deposited within Lake Ojibway II and is<br />

therefore very clayey.<br />

Cochrane Till may be overlain by a thin<br />

veneer of glaciolacustrine sediments<br />

similar to those which overlie the other<br />

till sheets.<br />

OJIBWAY II SEDIMENTS (Oil) (late Wisconsinan)<br />

glaciofluvial esker/delta sands and gravels<br />

glaciolacustrine fine sands, silts, clays<br />

(fining upward sequence - ice retreat)<br />

MATHESON TILL (MT) (Wisconsinan)<br />

pebbly, cobbly and/or bouldery tills with<br />

unsorted sandy, silty and locally clayey<br />

matrix<br />

commonly this unit will contain thin,<br />

discontinuous layers of sorted material<br />

MISSINAIBI SEDIMENTS (MS) (early Wisconsinan and Sangamon)<br />

Ojibway I glaciolacustrine sediments<br />

glaciofluvial sands and gravels<br />

LOWER TILL (LT) (Illinoian)<br />

pebbly, cobbly and/or bouldery tills with<br />

unsorted sandy, silty and locally clayey<br />

matrix<br />

OLDER SEDIMENTS AND TILLS (OS) ?<br />

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During advance and retreat of the main Wisconsinan ice sheet, the<br />

region was flooded by Lakes Ojibway I and II. Clay, silt and fine<br />

sands deposited at the lake bottom overlie both the Lower and<br />

Matheson Tills. Meltwater rivers that fed these lakes deposited<br />

glaciofluvial sands and gravels.<br />

In addition to the Quaternary stratigraphy, it is necessary to review<br />

our knowledge of the direction of the ice advances, since any<br />

dispersion train discovered would have to be traced back to its<br />

source.<br />

The most recent comprehensive study of ice-flow directions for this<br />

area was performed by Veillette (1986), who used cross-striated<br />

outcrop surfaces to determine relative ages and directions of ice<br />

flow. He concludes that:<br />

i) the ice direction during the last glacial maximum was<br />

south-southwest (180*-220*);<br />

ii) during late Wisconsinan time, a change in the ice flow direction<br />

occurred, towards the south-southeast (130 0 -170 0 );<br />

iii) striae trending west-southwest (230 0 -270 0 ) can be attributed to<br />

early Wisconsinan or pre-Wisconsinan glaciation.<br />

Veillette does not specifically discuss ice-flow directions for the<br />

Cochrane readvance, which affects only a minor section of the<br />

northern part of his study area. A review of airphotos in this area,<br />

together with a glance at the map of Boissoneau (1965), suggests<br />

though, that the Cochrane ice-flow direction here was close to 135*.<br />

In addition to the above information, we have recorded 78 striae<br />

measures on outcrops stripped during fall 1986. Of these, 69 fall<br />

between 125 0 and 150 0 with two additional measures at 160* (group ii<br />

above). One measure was taken at ISO 0 , and one at 190 0 (group i<br />

above) and four measures fall between 230 0 to 250* (group iii above).<br />

In the Burntbush area, then, the Lower Till ice direction may be at<br />

230 0 to 250 0 . Matheson Till ice-flow directions could range from<br />

125 0 to 190*, but striae trending 125 0 to ISO 0 may also be due in<br />

part, or in whole, to the Cochrane readvance.<br />

1.5 Bedrock <strong>Geology</strong> of the Burntbush River Project Area<br />

The bedrock geology of the area was first studied by Thomson (1936)<br />

and more recently by Johns (1982). The following brief summary<br />

serves only as an introduction; the reader is referred to our earlier<br />

reports for more detail (COGEMA Ref. Nos. 86-CND-47-02, 87-CND-47-01)<br />

and to section 4 of this report.<br />

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The property has been informally subdivided into a "northern low<br />

magnetic terrane" and "southern high magnetic terrane".<br />

Very few outcrops occur in the north part of the property, and from<br />

these it is interpreted that the area is underlain by predominantly<br />

high grade metasedimentary rocks (turbidites ?), with lesser<br />

predominantly mafic, metavolcanic rocks. A few intrusive metagabbros<br />

are present and there are numerous late dykes and veins of various<br />

compositions. On the east side, near the northern boundary, a high<br />

magnetic trend has been interpreted to be a sulfide facies iron<br />

formation.<br />

The southern part of the property appears to be less strongly<br />

metamorphosed than the northern part, and outcrop exposure is<br />

somewhat better. Tuffs and flows of mostly intermediate compositions<br />

have been mapped. These rocks have been intruded by various others,<br />

including metagabbros and diabase, but veining seems to be less<br />

common than in the north.<br />

It is believed that one or more major east-west structures transect<br />

the property and this is supported to some extent by our surface<br />

mapping.


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2. DESCRIPTION OF FIELD WORK<br />

2.1. Field Procedures<br />

This section details the field procedures adopted by the project<br />

personnel before, during and after the drilling of any overburden<br />

(reverse circulation) drill hole.<br />

Holes were spotted, and drill roads flagged by two-person teams.<br />

Using airphoto control, a 100 m nylon rope and compass, traverses<br />

were conducted. Drill roads were flagged and hole positions were<br />

marked with a picket and given a site number. In cases where dense<br />

bush or heavy deadfall were encountered, alternate access routes were<br />

flagged where possible.<br />

Linecutting started at about the same time as the hole spotting, and<br />

so cut lines were not completed in time to be of assistance in the<br />

hole positioning.<br />

Drilling required 5 persons. The driller, helper and water carrier<br />

ensured the smooth continuous running of the drill rig, and were<br />

together mechanically capable of keeping down-time to a minimum. A<br />

geologist and technician performed the logging and sampling. We used<br />

two teams of two persons during the winter program, and rotated the<br />

work between three persons during the summer program. During the<br />

first three weeks of the winter program, a consultant geologist from<br />

ODM was engaged (as a sixth person) to train us in the logging and<br />

sampling of the overburden and bedrock materials.<br />

The following text describes the logging criteria, and describes in<br />

detail each of the Quaternary units in order of appearance during a<br />

typical reverse circulation drill hole on the Burntbush River<br />

property.<br />

CT---Cp,chrane Till^and Sediments:)<br />

The Cochrane Till is a very clayey unit. The clay contains a<br />

few pebbles and rarely cobbles and/or boulders but always contains<br />

minor sand and granules. The sandy nature of the clay is evident<br />

when it is squeezed between the fingers. The unit is light brown to<br />

light grey in colour and the clay is soft. In the upper ~50 cm<br />

though, the clay may be fairly hard and compact and dark brown.<br />

Minor sandy sections with very little clay are not uncommon. In<br />

places, the till is overlain by a thin veneer of pure clay<br />

(glaciolacustrine sediments) similar to those units which overlie the<br />

older tills.<br />

- 8 -


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In the case of hole BOB-95, the Cochrane Till was very sandy and<br />

gravelly with only minor clayey sections because the hole was drilled<br />

very close to an esker which was slightly reworked by the Cochrane<br />

ice sheet.<br />

- kwa IISediments<br />

The Ojibway II Sediments comprise predominantly glaciolacustrine<br />

pure clays. The contact between these clays and the overlying clayey<br />

till is not abrupt and it is therefore probable that the contact has<br />

been logged deeper than it really is in some of the drill holes, i.e.<br />

Ojibway II clays are logged when the clay becomes pure, which is<br />

again evident when squeezed between the fingers. The clay is soft<br />

and light grey to bluish gray in colour.<br />

Fine sands and silts also represent a common overburden type<br />

logged as Ojibway II sediments. These generally underlie the pure<br />

clays or are interbedded with them. They are usually light brown in<br />

colour and are well sorted. Very minor coarse sand or pebbly<br />

interbeds may occur.<br />

In hole BOB-95, coarse sand and gravels are interpreted to<br />

represent an esker, part of the Ojibway II Sediments unit, which has<br />

no topographic relief due to later reworking by the Cochrane ice<br />

sheet.<br />

TiLl<br />

The Matheson Till underlies the above two units in nearly every<br />

hole drilled. The contact between this unit and the overlying<br />

Ojibway II Sediments (or Cochrane Till) is generally very abrupt.<br />

The coarse fraction of the Matheson Till unit is observed on a<br />

10 mesh screen and generally comprises pebble and cobble chips of<br />

various compositions. Most rock chips are coarse grained granitoids<br />

and metavolcanic and metasedimentary rocks. Generally, a few<br />

limestone clasts are encountered. These rock chips are logged in<br />

terms of their relative proportions over several metre intervals.<br />

Boulders are also commonly encountered and these are individually<br />

described.<br />

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The fine fraction of the till is described using a scoop. The<br />

fines generally consist of fine sands and silt of light grey-beige<br />

colour. Occasionally, the matrix of the till will be clayey due to<br />

reworking of the Ojibway I clays. In general, the Matheson Till is a<br />

poorly sorted, typical till unit, and it is therefore mostly<br />

described over several meter intervals.<br />

In some cases, sorted sand and gravel sections of limited depth<br />

extent are observed.<br />

MS---Miss.inaibi. Sediments,<br />

The Missinaibi Sediments unit as observed on the Burntbush River<br />

property comprises two members.<br />

Ojibway I pure gray clays have been encountered in a few drill<br />

holes. The clays are gray in colour and are generally compact and<br />

hard. When squeezed between the fingers they prove to be pure clay,<br />

but their compact nature requires some effort before they will<br />

compress. This is the only major difference between Ojibway I and<br />

Ojibway II clays. As with the younger (Ojibway II) glaciolacustrine<br />

unit, there may be sandy or pebbly interbeds of minor importance.<br />

Additionally, thick sections of sand and gravel have been<br />

encountered below the Matheson Till unit. These are heterogeneous.<br />

Coarse, medium and/or fine well sorted sands may be present or<br />

interbedded. Clean gravels with no supporting matrix may be<br />

encountered. Sandy gravels are also common and these may be<br />

difficult to distinguish from till. Careful attention must be paid<br />

when sandy gravels are being drilled due to their similarity to till,<br />

but generally some interbedding and/or sorting will be present to<br />

assist in their proper identification. There is also generally a<br />

very high rate of sample return when these materials are being<br />

drilled, which aids in identifying them.<br />

The Lower Till is in every respect similar to the Matheson<br />

Till. The only real field criteria which distinguishes it is the<br />

presence of the Missinaibi Sediments between the two till units.<br />

During reverse circulation drilling, it would be nearly impossible to<br />

distinguish it from Matheson Till if they were in contact with each<br />

other.<br />

- 10 -


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Field procedures for sampling the Quaternary units are as follows:<br />

1) The Matheson and Lower Tills are considered the most important<br />

sampling media, since it is these ice sheets which eroded the<br />

most bedrock, and would therefore be most likely to contain a<br />

gold bearing mechanical dispersion train.<br />

These tills are ideally sampled at 1.5 m intervals, since this<br />

length of sample most consistently gives an adequate quantity of<br />

sample material. And, more importantly, most dispersion trains<br />

are expected to have a minimum thickness of about 2 m at or very<br />

near to their source (eg at Golden Pond, Sauerbrei et al. 1987).<br />

With increasing transport distance, the anomaly should weaken<br />

but the thickness should increase. Thus, a dispersion train, if<br />

intersected, should give anomalous results in two (or more)<br />

adjacent overburden samples (within the same unit). Isolated,<br />

single sample anomalies must be very carefully evaluated before<br />

it is concluded that they represent a mechanical dispersion<br />

train.<br />

If, however, the sample return over a 1.5 m interval is<br />

considered insufficient, the sample length may be extended to 2<br />

or even 3 m.<br />

In most pebbly and cobbly sections, up to 75% of the rock chips<br />

which land on the 10 mesh screen are discarded. Thus, we<br />

attempt to sample predominantly the fine matrix material.<br />

Boulders are not sampled together with overburden materials,<br />

thus mixing of overburden and rock cuttings is avoided. In the<br />

event that a boulder is encountered and there is less than 1.5 m<br />

of overburden material in the sampling buckets, one of the three<br />

following procedures is adopted:<br />

i) if there is a sufficient quantity of material to give a<br />

sample of ~8 kg, the sample is taken as such, even though<br />

the sample interval is less than 1.5 m;<br />

ii)<br />

if there is an insufficient quantity of material, the<br />

previous (overlying) sample may be extended to a length of<br />

greater than 1.5 m, or<br />

iii) this material may be added to material sampled below the<br />

boulder to give a total sampled length of 1.5 m.<br />

- 11 -


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2) Sands and gravels which represent glaciofluvial deposits are<br />

also sampled, based on the premise that any Au anomaly found<br />

could be traced back to its source. However, these samples are<br />

considered of lower priority since the surface area of bedrock<br />

eroded by the glacio-fluvial systems would be much less.<br />

For this reason, sample intervals are generally greater,<br />

~3 m. Samples of shorter length have been taken, though, due<br />

to the high sample return in this overburden type.<br />

3) Fine sands of glaciolacustrine origin were occasionally sampled<br />

on the advice of the ODM consultant in the event that a placer<br />

deposit was present. This practice was discontinued after the<br />

winter program.<br />

4) The clayey Cochrane Till was not sampled, since it has eroded<br />

very little bedrock.<br />

In some cases, sandy sections of the Cochrane Till were<br />

sampled. This is due to its similarity in isolated cases to the<br />

Matheson Till. When very clayey till was re-entered, the<br />

geologist chose to retain the sample so as not to waste time<br />

rejecting it.<br />

5) Pure clays were never sampled, since there would be very little<br />

or no heavy mineral concentrate, and since the source area for<br />

these deposits could be several (hundreds of ?) kilometres away.<br />

After drilling the Quaternary section, bedrock is drilled for<br />

~1.5 m. The bedrock is briefly described using hand lens, lOH HC1,<br />

magnet, etc.<br />

Bedrock is sampled over 1.5 m and the hole is stopped at this point.<br />

Whereas the Quaternary section sample comprises mostly the fine<br />

materials, the bedrock sample is ideally comprised exclusively of<br />

chips, and the -10 mesh material is discarded.<br />

Also note that the occasional metasedimentary or metavolcanic boulder<br />

may be greater than 1.5 m in thickness. In isolated cases then, it<br />

is possible that a boulder has been sampled and called bedrock. No<br />

hole was stopped in a granite boulder of this size.<br />

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In some cases, due to caving in of overburden material around the<br />

rods, the bedrock sample was contaminated with foreign material.<br />

When the rock was soft enough that the bit advanced reasonably<br />

quickly, a good uncontaminated sample was obtained. For example in<br />

hole BOB-39, ~7 m of bedrock was drilled before a sample was<br />

taken. In cases where the bit advanced very slowly, a contaminated<br />

sample was taken.<br />

Such contaminated samples would be unsuitable for major element<br />

analyses, but should be suitable for Au geochemistry; any significant<br />

Au anomaly would, however have to be studied with this in mind.<br />

Most contamination of this type occurred in bedrock overlain by sands<br />

and gravels, which have a stronger tendency to cave in around the<br />

rods.<br />

Finally, in order to determine as precisely as possible the drill<br />

hole positions, we tied drill holes to the cut grid using chain and<br />

compass along the drill roads. In this manner, straight line<br />

distances of up to 100 m could be easily measured. Where drill roads<br />

cross the cut grid, the chainage on the cut grid at that point was<br />

used as a control. Where the same hole has been tied to the grid in<br />

two places, the calculated errors are generally less than 5 m (eg<br />

BOB-31 has been tied to BL04-00 at 2980E, and to L4900E at 666N).<br />

Additionally, claim posts which were visible from drill roads were<br />

tied to the cut grid in the same manner.<br />

2.2 Drilling and Sample Statistics<br />

In total, 133 different hole positions were drilled.<br />

information is provided in Table 2-1.<br />

Sample statistics are summarized in Table 2-2.<br />

Other pertinent<br />

A drilling summary is presented in Appendix I, as are the field<br />

logging sheets. Hap l shows the drill hole locations.<br />

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WINTER PROGRAM<br />

# of holes<br />

# of metres<br />

AVG HOLE DEPTH<br />

AVG DEPTH PER SHIFT*<br />

Table 2-1<br />

(BOB-01 to BOB-95)<br />

DRILLING STATISTICS<br />

95<br />

2034.5 MAXIMUM<br />

21.4 m 48.0 m<br />

61.6 m 100.8 m<br />

MINIMUM<br />

3.3 m<br />

29.3 m<br />

* excludes 22 and 23 March: drill was moved from hole BOB-39 to west side<br />

of river, hole BOB-40 was drilled - total depth 3.3 m - then drill was<br />

inoperative until 24 March when drilling was resumed.<br />

SUMMER PROGRAM<br />

it of holes<br />

# of metres<br />

AVG HOLE DEPTH<br />

AVG DEPTH PER SHIFT*<br />

(BOB-96 to BOB-133)<br />

39<br />

1124.5 MAXIMUM<br />

28.8 m 45.6 m<br />

66.1 m 102.4 m<br />

MINIMUM<br />

11.2 m<br />

24.0 m<br />

* excludes 6 July: drill was moved from hole BOB-130 to west side of river,<br />

no drilling was accomplished.<br />

CUMULATIVE RESULTS<br />

# of holes 134<br />

# of metres 3159<br />

AVG HOLE DEPTH<br />

AVG DEPTH PER SHIFT*<br />

23.6 m<br />

63.1 m<br />

* excludes 22 and 23 March, 6 July.<br />

- 14 -<br />

(BOB-125 drilled twice)


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A)<br />

Table 2-2<br />

SAMPLE STATISTICS<br />

OVERBURDEN SAMPLES (TO OVERBURDEN DRILLING MANAGEMENT LTD, HEAVY MINERAL<br />

CONCENTRATES TO CHIMITEC)<br />

WINTER PROGRAM<br />

Unit*<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

BK<br />

Total:<br />

SUMMER PROGRAM<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

(BOB-01 to BOB-95)<br />

ffi Samples Remarks<br />

5<br />

13<br />

527<br />

35.5 sample BOB-31-20 straddles contact<br />

69.5 between MS and LT<br />

1 sample BOB-37-23 (bedrock sent to<br />

wrong laboratory<br />

651<br />

3<br />

6<br />

376<br />

13<br />

12<br />

Total: 410<br />

B) BEDROCK SAMPLES (TO CHIMITEC)<br />

WINTER PROGRAM<br />

SUMMER PROGRAM<br />

TOTAL:<br />

(BOB-96 to BOB- 133)<br />

98<br />

43<br />

* This compilation based on field designations equivalent to those<br />

given in the Drilling Summary and on Drill Hole Sections, but see<br />

also Section 3.1 in text.<br />

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3. OVERBURDEN RESULTS<br />

3.1 Presentation of Drill Hole Sections<br />

The first objective of the drill hole sections is to show the local<br />

Quaternary stratigraphy (Maps 2 to 9; see Map l for key to sections).<br />

Although a few minor changes were made to the field logs based on<br />

hole to hole correlations during their construction, the stratigraphy<br />

presented is essentially a field interpretation.<br />

The drill holes are plotted at nominal distances of 400 m (for most<br />

holes) and 200 m (for follow-up holes) and not at their precise<br />

positions as determined by chaining. The collar elevations were<br />

estimated from the topographic map and from field notes.<br />

From these sections, the following introductory remarks are drawn:<br />

i) overburden depths on the east side of the Burntbush River are,<br />

on average, greater than on the west side (see also Fig. 3-1).<br />

This confirms our previous interpretation using airborne VLF-EM<br />

results, and justifies our having traversed this area at greater<br />

spacing during the summer 1986 field season (see COGEMA Ref.<br />

No. 86-CND-47-02).<br />

ii) this thicker overburden is due mostly to a thick blanket of<br />

till. We had previously thought that the thicker overburden<br />

would be due to glaciolacustrine clays, as is the case on many<br />

properties in the "Casa Berardi area".<br />

iii) a thin veneer of Cochrane Till is everywhere present. This<br />

result was not expected, most maps published up to now draw the<br />

limit of the Cochrane advance just north of the property.<br />

However, we have previously reported that boulders and cobbles<br />

"are numerous and can be found almost anywhere when the grubhoe<br />

is used diligently" (COGEMA Ref. No. 86-CND-47-02, p.8),<br />

indicating that this could have been deduced earlier.<br />

iv) pre-Wisconsinan units (Missinaibi Sediments and Lower Till) were<br />

logged in several holes, mostly on the eastern side of the<br />

property.<br />

Further discussion of this last remark is necessary, and important<br />

revisions of the field interpretations are presented below. These<br />

revisions have not been indicated on the drill sections, which were<br />

previously noted to represent field interpretations.<br />

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Figure 3-1 :<br />

Overburden Thicknesses on the Burntbush River<br />

Property.<br />

Scale 1:40 000<br />

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For example, on section G-G' (Map 8), we have logged Lower Till in<br />

holes BOB-89, 90, 91 and 93. This interpretation is suspect for<br />

three reasons: 1) Lower Till is known to be preserved generally only<br />

in deep bedrock depressions, preferably oriented ~ east-west, 2)<br />

the two tills are separated by only a thin veneer of sediments, and<br />

furthermore, 3) in hole BOB-90, the "Lower Till" is underlain by more<br />

sediments. It is probable that this thin unit of sediments indicates<br />

a minor interstadial period, and that the main Wisconsinan ice sheet<br />

retreated briefly from this area.<br />

Further evidence of a minor retreat and subsequent readvance is<br />

present on the east side of the river, and is illustrated by a<br />

north-south section including holes BOB-125, 33, 21 and 22 (see Fig.<br />

3-2). On this section, we drilled abundant fine sands, thought to be<br />

of glaciolacustrine origin (note the fining upward sequence in the.<br />

southern part). It is now possible to recognize on the airphotos,<br />

though, a weakly developed esker north of hole BOB-125. This esker<br />

has been partly reworked and in hole BOB-21, we are able to see the<br />

buried esker, a till overlying it, and sediments deposited by the<br />

rejuvenated esker near the top of the section.<br />

This esker appears to be of late-Wisconsinan, but pre-Cochrane age.<br />

Most Cochrane eskers near here trend close to southeast (eg just west<br />

of the Burntbush River, see Map 4 in COGEMA Ref. No. 86-CND-47-02),<br />

whereas this esker trends close to north-south and is overlain by a<br />

thin veneer of Cochrane Till.<br />

We conclude from these results that two tills of Wisconsinan age<br />

(excluding the very late Wisconsinan Cochrane Till) have been drilled<br />

on the property. The older Wisconsinan till may correlate with<br />

"classical" Matheson Till, while the younger till would be due to a<br />

minor late Wisconsinan readvance. These results seem to agree with<br />

those of Veillette (1986), who proposes a shift in ice-flow direction<br />

in late Wisconsinan time. Perhaps this change in ice-flow direction<br />

correlates with this late Wisconsinan readvance.<br />

Lower Till interpreted to occur in drill holes adjacent to this<br />

section (holes BOB-23, 24, 25, 31, 32, 34, 124, 126, 128, 129) may<br />

therefore be re-interpreted as Matheson Till.<br />

A second buried esker of Wisconsinan age might also be postulated<br />

just west of Nedlog Lake (holes BOB-36, 37, 104, 107, 109) on similar<br />

grounds, but with no subsequent development of a "rejuvenated" esker.<br />

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Figure 3-2 : Drill Section L-L'. See Map l for section<br />

location. Horizontal scale 1:5000, vertical<br />

scale 1:500, vertical exaggeration 10X.<br />

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Other holes which were thought to contain Lower Till are BOB-01, 02<br />

and 12. It is now believed that the Lower Till in hole BOB-12 are<br />

sands and gravels similar to those logged in the adjacent hole<br />

BOB-114. Due to the significant numbers of gold grains in these<br />

holes (see next section), these samples were studied under the<br />

binocular microscope by S. Averill (of ODM) and he confirms them to<br />

be such. In the area of holes BOB-01 and 02, a glance at section<br />

A-A' shows that Ojibway II clays in hole BOB-04 are at the same<br />

elevation as "Ojibway I" clays in these two holes. Thus, a late<br />

Wisconsinan till overlies Ojibway II clays in holes BOB-01 and 02.<br />

In summary, it seems very probable that no Lower Till was intersected<br />

in our drilling, and that two Matheson Tills are present. Much of<br />

the sands and gravels drilled are part of the Ojibway II<br />

glaciofluvial unit, and not of pre-Wisconsinan age. Perhaps the only<br />

pre-Wisconsinan materials drilled on the property are in the lower<br />

sections of holes BOB-12, 114 and 115 (Missinaibi Sediments glacio<br />

fluvial unit), where the steepest bedrock topography is present.<br />

3.2 Sample Results<br />

Our overburden samples were sent to ODM laboratories in Nepean, Ont.<br />

(holes BOB-01 to BOB-95, winter program) and Rouyn, Que. (holes<br />

BOB-96 to BOB-133, summer program). This initial sample treatment<br />

yields a variety of data (see Appendix II for a procedural summary<br />

and a full listing of their results) but the most important work they<br />

perform is gold grain counts and the preparation of a heavy mineral<br />

concentrate (HMC).<br />

The purpose of gold grain counts is to detect by physical means any<br />

mechanical dispersion train present. The HMC is analyzed in an<br />

effort to detect gold which is too fine to physically (visually)<br />

detect, and/or to check for fine gold occluded in sulfide minerals.<br />

Commonly, though, a high gold value in the HMC is due to a single<br />

coarse grain (nugget effect) and the gold grain count can eliminate<br />

most of these "anomalies" at an early stage.<br />

The results of the gold grain counts (raw data) have been added to<br />

the field logs and are plotted on the drill sections. Also, the<br />

results are summarized in Table 3-1 and a plan map showing the total<br />

number of gold grains found in all samples of each drill hole is<br />

shown in Figure 3-3.<br />

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Table 3-1<br />

ffi samples (overburden) 650<br />

ffi samples with Au grains 188 (29%)<br />

ffi Au grains 361<br />

GOLD GRAIN COUNTS - A SUMMARY<br />

WINTER PROGRAM (BOB-01 to BOB-95)<br />

Average ffi Au grains/sample having Au grains 1.9<br />

ffi of samples with l Au grain 132<br />

ffi of samples with 2-4 Au grains 41<br />

(207o of total samples)<br />

(70X of samples with Au grains)<br />

C 6% of total samples)<br />

(227o of samples with Au grains)<br />

ffi of samples with 5 or more Au grains 15 ( 2% of total samples)<br />

(2 samples have more than 10 grains) ( 8% of samples with Au grains)<br />

ffi samples (overburden) 410<br />

ffi samples with Au grains 218 (537.)<br />

ffi Au grains 560<br />

SUMMER PROGRAM (BOB-96 to BOB-133)<br />

Average ffi Au grains/sample having Au grains 2,6<br />

of samples with l Au grain 120<br />

of samples with 2-4 Au grains 55<br />

(29% of total samples)<br />

(55* of samples with Au grains)<br />

(13* of total samples)<br />

(25% of samples with Au grains)<br />

ffi of sample with 5 or more Au grains 43 (11* of total samples)<br />

(no samples have more than 10 grains) (20% of samples with Au grains)<br />

- 21 -


Figure 3-3 :<br />

Total Gold Grain Counts for Overburden<br />

Drill Holes. Scale 1:40 000<br />

- 22 -


l l l l l l<br />

l l l l l l l<br />

l l l l l<br />

l<br />

From Table 3-1, we see that significantly more gold grains were<br />

counted (relative to the number of samples taken) from the summer<br />

program (Rouyn lab) compared to the winter program (Nepean lab).<br />

This makes comparison of results from the two programs more difficult.<br />

We might suggest that samples from the winter program carrying 2 or<br />

more gold grains (87. of total samples) are equivalent to samples from<br />

the summer program which carry 5 or more gold grains (lilt of total<br />

samples). Meanwhile, Figure 3-3 shows that there is some correlation<br />

between total gold grain counts and overburden thickness (compare<br />

with Figure 3-1). Thicker overburden sections are producing higher<br />

total grain counts.<br />

As noted in Appendix II, the gold grains are eventually returned to<br />

the non-magnetic portion of the HMC. But first, the dimensions of<br />

each grain are recorded, and from this a "calculated ppb" is<br />

estimated for each sample. This value can be compared with the<br />

analytical result to help identify those results which are due to<br />

free gold only from those which might be due to fine and/or occluded<br />

gold (see later).<br />

Using the grain dimensions, we have constructed comparative<br />

histograms of gold grain volumes counted in the Nepean and Rouyn<br />

laboratories. Figure 3-4 shows that the Rouyn lab was capable of<br />

detecting more fine gold than the Nepean lab, which helps explain the<br />

differences observed in Table 3-1.<br />

Also, the form (degree of rounding) of each individual grain is<br />

recorded. The form of a gold grain is believed to be related to its<br />

distance of transport (Averill and Zimmerman, 1986; see Fig. 3-5).<br />

This concept does not take into consideration the possibility of a<br />

gold grain being released from a boulder already removed from its<br />

source, nor are the stated transport distances particularly well<br />

documented.<br />

Of 926 gold grains counted in overburden samples from the two<br />

programs, nearly every grain was abraded. No rounded grains were<br />

found, thirty-one grains were classed as irregular and four grains<br />

were classed as delicate. Figure 3-6 shows the distribution of<br />

irregular and delicate grains.<br />

After these studies are completed, and when the HMC is ready for<br />

analysis, the sample is split into two parts, and one part is sent to<br />

CHIMITEC Ltee. The non-magnetic HMC is analyzed by neutron<br />

activation for Au plus 33 other elements and for Cu by atomic<br />

absorption. A procedural summary and a complete listing of results<br />

is given in Appendix III.<br />

- 23 -


l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Figure 3-4<br />

Comparative Histograms of Gold Grain Volumes<br />

Reported by ODM from the Winter {Nepean lab)<br />

and Summer (Rouyn lab) Programs. The volumes<br />

are in Iny 3 (natural logarithm of the product<br />

of the three estimated dimensions of each grain)<br />

The vertical (frequency) scale is l grain/mm<br />

- 24 -


DELICATE<br />

0-100 m ice transport.<br />

Primary crystal faces, pitted leaf<br />

surfaces tt ragged leaf edges intact.<br />

IRREGULAR<br />

100-1000 m ice transport<br />

Gross primary shape<br />

and pitted surface<br />

intact.<br />

IRREGULAR<br />

Curled leaf variety.<br />

ABRADED<br />

1000+ m ice transport.<br />

Large primary leaf<br />

reduced to smaller<br />

flakes with polished<br />

surfaces.<br />

ABRADED<br />

Spindled leaf variety.<br />

O<br />

ROUNDED<br />

1000+ m ice * stream transport.<br />

Polished equidimensional grains.<br />

Figure 3-5 :<br />

Effects of Glacial Transport on Gold Particle<br />

Size and Shape (Developed by ODM)<br />

- 25 -


s l irregular grain<br />

O<br />

= l delicate grain<br />

indicates sample near base<br />

of Quaternary Section<br />

Figure 3-6 :<br />

Distribution of Irregular and Delicate Gold<br />

Grains. Scale 1:40 000<br />

- 26 -


l l l l l l<br />

l l l l l l l<br />

l l l<br />

l l l<br />

Au results range from very low (below detection limits) to 24 900 ppb<br />

(sample BOB-122-03). Although this result sounds very interesting,<br />

it is due mostly to a single coarse abraded nugget detected during<br />

sample treatment. The "calculated ppb" of this nugget is 21 204<br />

ppb. This is an example of the precision between "calculated" and<br />

analytical results. In fact, a correlation coefficient of 0.85 was<br />

obtained when "calculated" and analytical results for gold were<br />

compared (for samples carrying detected gold grains).<br />

The high correlation is even more surprising When we consider the<br />

implications of the actual procedures involved. Remember that the<br />

HMC is split into a 3/4 (analyzed) fraction and a 1/4 (retained)<br />

fraction. Some of the gold grains are certain to fall into the<br />

retained fraction such as probably happened in the case of sample<br />

BOB-56-03 where the "calculated ppb" was 9443 ppb and the analytical<br />

result was 794 ppb (total of 5 gold grains summed in "calculated<br />

ppb").<br />

The other elements analyzed for are listed in Table 3-2. Of all of<br />

these, As seems to give the only meaningful results for this program.<br />

The first evidence of this are the contrasting As values in holes<br />

BOB-01 and 02 from two different till sheets separated by a glacio<br />

lacustrine clay horizon. Table 3-3 summarizes these results.<br />

- 27 -


1<br />

1 Table 3-2 : SUMMARY OF THE OTHER ELEMENTS ANALYZED FOR<br />

<br />

IN HEAVY MINERAL CONCENTRATES<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

ELEMENT<br />

Sb<br />

As<br />

Ba<br />

Cd<br />

Cs<br />

Gr<br />

Co<br />

Eu<br />

Hf<br />

Ir<br />

Fe<br />

MEAN*<br />

0.5<br />

27.5<br />

146<br />

16<br />

1.3<br />

871<br />

125<br />

8<br />

251<br />

22.4<br />

STANDARD<br />

DEVIATION<br />

0.2<br />

36.2<br />

45<br />

7<br />

0.5<br />

158<br />

63<br />

2<br />

69<br />

2.5<br />

N*<br />

982<br />

940<br />

63<br />

39<br />

94<br />

1060<br />

1060<br />

1060<br />

1060<br />

0<br />

1060<br />

DETECTION<br />

LIMIT<br />

- 28 -<br />

0.1 ppm<br />

0.5 ppm<br />

50 ppm<br />

5 ppm<br />

0.5 ppm<br />

20 ppm<br />

5 ppm<br />

1 ppra<br />

1 ppm<br />

50 ppm<br />

D.2%<br />

COMMENT!<br />

no anomalous resu!<br />

ciated with high i<br />

results too unifoi<br />

useful<br />

no anomalous resu<br />

ciated with high i<br />

probable stratign<br />

to separate two W:<br />

tills<br />

too few results at<br />

detection limit<br />

too few results at<br />

detection limit<br />

too few results at<br />

detection limit<br />

could be tested fc<br />

tigraphic use<br />

could be tested f c<br />

tigraphic use<br />

results too unifot<br />

useful<br />

could be tested fc<br />

tigraphic use, hig<br />

relation with Zr,<br />

no results above<br />

detection limit<br />

could be tested fc<br />

tigraphic use<br />

(cor


l l l l<br />

l l<br />

l l l l l l l<br />

l l l l l<br />

l<br />

(cont'd)<br />

ELEMENT<br />

La<br />

Mo<br />

Ni<br />

Rb<br />

Se<br />

Se<br />

Ag<br />

Ta<br />

Tb<br />

Th<br />

Table 3-2 : SUMMARY OF THE OTHER ELEMENTS ANALYZED FOR<br />

IN HEAVY MINERAL CONCENTRATES<br />

MEAN*<br />

423<br />

5<br />

94<br />

19<br />

87.7<br />

14<br />

9<br />

24.2<br />

8.7<br />

188.5<br />

STANDARD<br />

DEVIATION<br />

126<br />

7<br />

45<br />

8<br />

10.7<br />

1<br />

0<br />

26.3<br />

1.7<br />

73.6<br />

N*<br />

1060<br />

456<br />

939<br />

257<br />

1060<br />

2<br />

1<br />

1060<br />

1060<br />

1060<br />

DETECTION<br />

LIMIT<br />

- 29 -<br />

2 ppm<br />

1 ppm<br />

20 ppm<br />

5 ppm<br />

0.2 ppm<br />

5 ppm<br />

2 ppm<br />

0.5 ppm<br />

0.5 ppm<br />

0.2 ppm<br />

COMMENTS<br />

could be tested for stra<br />

tigraphic use, high cor<br />

relation with Th, Ce, Tb,<br />

Yb, Lu<br />

no anomalous results asso<br />

ciated with high Au values,<br />

most results below detec<br />

tion limit<br />

could be tested for stra<br />

tigraphic use<br />

most results below<br />

detection limit<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with Yb<br />

too few results above<br />

detection limit<br />

too few results above<br />

detection limit<br />

could be tested for stra<br />

tigraphic use<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with La, Th, Ce, U,<br />

Yb, Lu<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with La, Ce, Tb, U,<br />

Yb, Lu<br />

(cont'd)


l l l l l<br />

l<br />

l l<br />

l l l l l l l l<br />

l l<br />

l<br />

(confd)<br />

ELEMENT<br />

W<br />

U<br />

Yb<br />

Zn<br />

Ce<br />

Na<br />

Sn<br />

Te<br />

Zr<br />

Table 3-2 : SUMMARY OF THE OTHER ELEMENTS ANALYZED FOR<br />

IN HEAVY MINERAL CONCENTRATES<br />

MEAN*<br />

46<br />

21.7<br />

32<br />

177<br />

745<br />

0.38<br />

245<br />

41<br />

12330<br />

STANDARD<br />

DEVIATION<br />

115<br />

4.9<br />

5<br />

46<br />

214<br />

0.26<br />

74<br />

13<br />

3319<br />

N*<br />

864<br />

1059<br />

1059<br />

695<br />

1060<br />

756<br />

422<br />

321<br />

1060<br />

DETECTION<br />

LIMIT<br />

- 30 -<br />

1 ppm<br />

0.2 ppm<br />

2 ppm<br />

100 ppm<br />

5 ppm<br />

G.02%<br />

100 ppm<br />

10 ppm<br />

200 ppm<br />

COMMENTS<br />

some high results in<br />

Missinaibi gravels with Au,<br />

danger of contamination<br />

from tungsten carbide drill<br />

bits<br />

could be tested for stra<br />

tigraphic use high corre<br />

lation with Hf , Zr, Th, Tb<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with Lu, Ce, La, Th,<br />

Tb, Se<br />

no anomalous results asso<br />

ciated with high Au values,<br />

could be tested for strati<br />

graphic use<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with La, Th, Tb, Lu,<br />

Yb<br />

could be tested for strati<br />

graphic use<br />

no anomalous results asso<br />

ciated with high Au values,<br />

most results below detec<br />

tion limit<br />

no anomalous results asso<br />

ciated with high Au values,<br />

most results below detec<br />

tion limit<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with Hf , U<br />

(cont'd)


l l l l l l<br />

l l l l l l l l l l l l<br />

l<br />

(cont'd)<br />

ELEMENT<br />

Br<br />

Lu<br />

Sm<br />

Cu<br />

Table 3-2 : SUMMARY OF THE OTHER ELEMENTS ANALYZED FOR<br />

IN HEAVY MINERAL CONCENTRATES<br />

MEAN*<br />

5.9<br />

5.3<br />

62.14<br />

115<br />

STANDARD<br />

DEVIATION<br />

3.2<br />

0.9<br />

18.73<br />

71<br />

N*<br />

574<br />

1059<br />

1060<br />

1060<br />

DETECTION<br />

LIMIT<br />

0.5 ppm<br />

0.2 ppm<br />

0.05 ppm<br />

1 ppm<br />

COMMENTS<br />

could be tested for stra<br />

tigraphic use<br />

could be tested for stra<br />

tigraphic use, high corre<br />

lation with Yb, Ce, La, Th,<br />

Tb<br />

could be tested for stra<br />

tigraphic use<br />

no anomalous results asso<br />

ciated with high Au values,<br />

could be tested for stra<br />

tigraphic use<br />

* arithmetic mean used; only results above detection<br />

limit used in this table, N = number of results<br />

above detection limit; total number of samples is<br />

1060.<br />

- 31 -


l l l l<br />

l l<br />

l l l l<br />

l l l<br />

l l l l l<br />

l<br />

Table 3-3<br />

YOUNGER TILL<br />

Sample #<br />

01-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

OLDER TILL<br />

Sample #<br />

01-06<br />

-07<br />

-08<br />

-09<br />

As RESULTS FROM HEAVY MINERAL CONCENTRATES<br />

FROM TWO TILLS IN HOLES BOB-01 and BOB-02<br />

As<br />

As<br />

(ppm)<br />

2<br />

3.9<br />

22<br />

16<br />

78<br />

(ppm)<br />

98.8<br />

57.8<br />

68.5<br />

73.4<br />

- 32 -<br />

Sample<br />

02-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

Sample<br />

02-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

# As (ppm)<br />

7<br />

28<br />

33<br />

34<br />

16<br />

# As (ppm)<br />

38<br />

91.6<br />

196<br />

49<br />

54.8


l l l l l l<br />

l l l l l l l l<br />

l l l l<br />

l<br />

3.3 Discussion of Background and Threshold Values<br />

Our reverse circulation program generated 1060 overburden samples.<br />

This is a large amount of data, most of which, in all probability<br />

represent background results. This section discusses how we might<br />

differentiate background results from those which are, or may be,<br />

indicative of a mechanical dispersion train.<br />

Background and threshold values for gold grains in tills of the<br />

northern Abitibi are suggested to be between 200 and 500 grains/m^,<br />

and 2500 grains/m^, respectively (Averill, 1988). Most of our<br />

overburden samples weighed 8 to 10 kg and had an approximate volume<br />

of 0.004 to 0.005 m3 . Background till samples would then be<br />

expected to carry 0.8 to 2.5 gold grains (assuming all of the gold<br />

grains are detected). Similarly, the threshold value can be<br />

calculated to be approximately 10 gold grains per sample.<br />

Some published literature describes mechanical gold dispersion from<br />

known bedrock occurrences. In all cases, there is little discussion<br />

of actual background and threshold values, but examples of anomalous<br />

results are given.<br />

Averill and Zimmerman (1984) discovered a dispersion train which led<br />

to the discovery of the EP zone at Waddy Lake, Saskatchewan. They<br />

used 10 gold grains per sample as a threshold value, but the<br />

dispersion train they describe contained 100 gold grains per sample.<br />

These samples had HMC assay values of ^00 000 ppb Au.<br />

Sauerbrei et al (1987) drilled reverse circulation holes up-ice and<br />

down-ice from the Golden Pond discovery in Casa Berardi Township,<br />

Quebec. They were able to detect mechanical dispersion of gold in<br />

till down-ice from the deposit. They later used the method to test<br />

the strike extension of the mineralization and found new anomalies<br />

which led to the discovery of the Golden Pond East and West zones.<br />

One anomalous sample they describe contained approximately 700<br />

delicate gold grains and assayed 106 000 ppb Au (in the HMC). This<br />

sample proved to be directly adjacent to bedrock mineralization. A<br />

much less spectacular result taken at about 400 m down-ice from the<br />

deposits contained 7 abraded and 2 irregular grains and assayed 9100<br />

ppb Au (in the HMC).<br />

They also note that most anomalous samples also gave high As values<br />

(eg 3060 to 140 000 ppm) and oversized HMCs, rich in pyrite and<br />

arsenopyrite (eg 100 g concentrates rather than 10 to 30 g for<br />

background samples).<br />

- 33 -


l l l l l l<br />

l l l l l l l l l l l l<br />

l<br />

Finally, for gold assays in the HMCs, one of their figures describes<br />

results ^000 ppb as being anomalous, 500-2000 ppb as weakly<br />

anomalous and ^00 ppb as non-anomalous. However, they acknowledge<br />

that erratic, isolated values higher up in the Quaternary section are<br />

probably not related to the bedrock mineralization.<br />

Some published studies give HMC results but do not give gold grain<br />

count results. Harron et al (1987) contoured anomalous HMC assays at<br />

2000 ppb Au and noted results as high as 19 000 ppb for a program<br />

near Timmins, Ont. Gleeson and Sheehan (1987) suggested lower<br />

threshold values be used at the Doyon and Bousquet deposits but their<br />

heavy liquid density was 2.96 (compared to 3.3 for most programs).<br />

In summary, very strongly anomalous till samples should be easy to<br />

distinguish. However, criteria to separate weakly anomalous samples<br />

(truly indicative of bedrock mineralization) from background samples<br />

(especially high background samples) of no value are poorly defined.<br />

3.4 Interpretation of Overburden Results<br />

None of our samples can be described as strongly anomalous. No<br />

samples contained abundant delicate or irregular gold grains. Most<br />

of the high assays for gold are due to a single coarse gold grain<br />

which cannot be presumed to indicate nearby bedrock mineralization.<br />

Associated elements results (eg As, Cu, Zn, Sb) are low and do not<br />

correlate with the Au results. No oversized HMCs rich in metallic<br />

minerals were found.<br />

We have, however, discovered that two Wisconsinan tills (excluding<br />

Cochrane Till) are present on the property. The younger till was<br />

probably deposited close to the ice front of a minor readvance during<br />

late Wisconsinan time. If true, this ice sheet would have been less<br />

thick and would have been less capable of significantly eroding the<br />

bedrock surface. Therefore, we could postulate that a mechanical<br />

dispersion train in this late till might be less evident than in some<br />

of the examples reviewed.<br />

For this reason, we have chosen the following threshold values:<br />

i) minimum 5 gold grains per sample, or<br />

ii) ^00 ppb Au in the HMC.<br />

Out of the total 1060 samples taken, 194 were selected for further<br />

examination using these criteria. Most were eliminated as<br />

non-anomalous based on the following observations:<br />

- 34 -


1<br />

I.*<br />

1 1111111111111111<br />

i)<br />

Many high HHC results are due to the presence of a single<br />

coarse (eg ^00 ppb) gold grain. Such coarse grains<br />

occur erratically in tills (Averill, 1988). A few samples<br />

even contained two coarse (eg ^00 ppb) , abraded gold<br />

grains.<br />

ii) In other cases, a moderately high HMC result was shown to<br />

be due to well-travelled, background grains not coarse<br />

enough to (by themselves) cause a 500 ppb result.<br />

iii) Isolated high HMC results from the near-surface in areas of<br />

thick overburden were assumed to be caused by background<br />

grains (or, perhaps, a single coarse nugget) that were not<br />

detected during sample treatment.<br />

iv) Samples with more than 5 grains but with HMC results ^00<br />

ppb were also eliminated and interpreted to be high<br />

background samples. Most of these samples have only 5 to 7<br />

grains and were drilled in summer (Rouyn lab) .<br />

Using these guidelines, nearly all of the 194 samples were classed as<br />

non-anomalous , high background or erratic values. A few samples,<br />

though, could not be easily rejected and these were classed as<br />

possibly anomalous. In most cases, analyses of the 1/4 (retained)<br />

split of these samples was requested. All possibly anomalous samples<br />

are discussed below, and results of the second analyses are given.<br />

Area 1 (east of Blue Lake)<br />

HMC<br />

Sample it tt gold grains calc ppb<br />

(of sold Rrains)<br />

assay ppb<br />

(3/4 split)<br />

2nd assay ppb<br />

(1/4 split)<br />

BOB-06-02 2 2877 7410 23<br />

BOB-07-05 0 0 1850 622<br />

BOB-02-09 1 2539 1090 -(18<br />

BOB-04-03 1 4296 1600<br />

Each of these samples was taken at or near the base of the Quaternary<br />

section. Stratigraphic considerations and As geochemistry suggest<br />

that the samples come from the older Matheson Till.<br />

Hole BOB-06 is located southeast of a short electromagnetic conductor<br />

which was drilled in 1976 by Geophysical Engineering Ltd. A few<br />

short sections of massive pyrrhotite and pyrite were drilled along<br />

with quartz and quartz-carbonate veins. Assays over 8 to 13 foot<br />

lengths (2.4 to 4.0 m) returned "nil" gold values.<br />

- 35 -


l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

The basal sample from hole BOB-06 contained two gold grains; both are<br />

abraded and one is very coarse (accounting for 2527 ppb by itself).<br />

Both gold grains are probably well-travelled background grains, but<br />

the HHC assay is quite high relative to the expected result. Since<br />

the HMC was rich in pyrite (~35%), the high result may be due to<br />

fine or occluded gold. Analysis of the 1/4 split gave a result of 23<br />

ppb. This suggests that no fine or occluded gold is present in the<br />

sample, i.e. the calculated ppb of the detected grains was underesti<br />

mated, or an additional coarse grain was missed during sample<br />

treatment.<br />

Hole BOB-07 (located at ~400 m west-southwest of hole BOB-06) gave<br />

one sample with a HHC result of 1850 ppb, but contained no visible<br />

gold and very few sulfide minerals. A second analysis was requested<br />

to determine whether the result was erratic (i.e. due to undetected<br />

gold grain(s), or was perhaps due to abundant fine gold. This second<br />

analysis gave a result of 622 ppb. Although this result is higher<br />

than the threshold of 500 ppb which we used, it is much lower than<br />

the first analysis. This strongly suggests that a few background<br />

gold grains were missed during sample treatment. This sample,<br />

though, is classed as possibly anomalous as it may be indicative of a<br />

weak dispersion train carrying fine gold.<br />

Holes BOB-02 and BOB-04 are at ~400 m down-ice from holes BOB-06<br />

and BOB-07, respectively. In both cases, the HMC result is much<br />

lower than the expected value estimated from the volume of single<br />

coarse grains. The low value may indicate that the coarse grains<br />

remained in the 1/4 split, and that abundant fine gold (or an<br />

undetected second coarse grain) is present in the sample.<br />

Alternatively, the low assay may be due to an imprecise volume<br />

estimate and/or INA shielding. A second assay on sample BOB-02-09<br />

gave a result of •GLS ppb. This result shows that no fine gold<br />

anomaly is present.<br />

- 36 -


l l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

Area 2 (northeast corner of Blue Lake)<br />

HHC<br />

Sample # it of gold grains calc ppb assay ppb<br />

BOB-12-09 8 3260 1490<br />

BOB-12-12 19 7568 6020<br />

BOB-12-15 7 489 373<br />

BOB-12-16 13 593 868<br />

BOB-12-17 l 82 764<br />

BOB-114-09 4 2561 1490<br />

BOB-114-10 8 1006 160<br />

BOB-114-11 3 794 1390<br />

BOB-114-12 6 1216 1900<br />

BOB-115-15 l 291 5360<br />

These samples were taken from buried glaciofluvial sands and gravels<br />

of pre-Wisconsinan age (Missinaibi Sediments), except BOB-12-09 which<br />

is a basal till sample of the same (slightly reworked) material. All<br />

of the discussion presented on background and thresholds deals with<br />

tills, and we are not certain that similar thresholds can be applied<br />

to this unit.<br />

Most of the gold grains in these samples are relatively coarse and of<br />

uniform size. These samples suggest the presence of a low grade,<br />

buried placer deposit. It is not improbable that coarse gold of<br />

unknown provenance was concentrated out of older tills into these<br />

gravels.<br />

Due, however, to the restricted distribution of these sediments, and<br />

the local steep bedrock topography, it might be unwise to<br />

categorically conclude that these results have no exploration<br />

significance.<br />

Area 3 (west-northwest of camp)<br />

HMC<br />

Sample # //of gold grains calc ppb assay ppb 2nd assay ppb<br />

BOB-93-04 7 1092 1110 160<br />

BOB-94-07 3 360 1100 180<br />

BOB-132-05 l 2608 1420 56<br />

BOB-58-03 O O 1520<br />

- 37 -


l l l l<br />

l l<br />

l l l l l l l l l l l l<br />

l<br />

These samples were all taken at or near the base of the Quaternary<br />

section. As geochemistry might suggest that these samples come from<br />

the younger, late Wisconsinan till.<br />

Sample BOB-94-07 contained 3 gold grains of similar grain size, and<br />

all were classed by ODH as irregular. The HMC assay result was<br />

higher than expected, and so a second analysis was requested. The<br />

new result is 180 ppb.<br />

Sample 93-04 contained 5 abraded and 2 irregular grains and is<br />

located 400 m west of hole BOB-94. This sample contains aim<br />

section of sorted sandy gravelly material, which renders<br />

interpretation of the result more difficult. However, a second<br />

analysis was requested which gave a result of 160 ppb.<br />

Second analyses were also requested from BOB-58-03 and 132-05.<br />

results also show low values.<br />

We interpret from these results that no important dispersion train<br />

has been intersected in this area.<br />

Other possibly anomalous samples<br />

Sample tt<br />

BOB-34-12<br />

BOB-34-15<br />

BOB-64-03<br />

BOB-74-02<br />

BOB-86-05<br />

BOB-89-09<br />

BOB-101-14<br />

BOB-104-18<br />

of gold Rrains calc ppb<br />

O<br />

0<br />

O<br />

0<br />

O<br />

0<br />

l<br />

587<br />

4<br />

2749<br />

O<br />

0<br />

4<br />

514<br />

7 703<br />

HMC<br />

assay ppb<br />

1600<br />

1470<br />

5400<br />

1240<br />

3300<br />

2500<br />

1030<br />

1450<br />

These<br />

2nd assay ppb<br />

25<br />

41<br />

^0<br />

29<br />

59<br />

O.8<br />

590<br />

43<br />

These samples come from at or near the base of the Quaternary section<br />

and are scattered (more or less) across the property. Second<br />

analyses of the 1/4 split were requested to check for the possibility<br />

of abundant fine gold. In all cases except one, the second analysis<br />

gives a very low result which rules out the possibility of a fine<br />

gold anomaly. But, similar to sample BOB-07-05 (discussed earlier),<br />

sample BOB-101-14 gives a result over 500 ppb, but significantly<br />

lower than the first analysis. This sample is classed as possibly<br />

anomalous.<br />

- 38 -


l l l l<br />

l l<br />

l l l<br />

l l<br />

l l l l l l<br />

l<br />

l<br />

In summary, the results of the overburden sampling show no clearly<br />

defined anomalies. The best results come from Missinaibi sands and<br />

gravels from northeast of Blue Lake. But, since we have very limited<br />

data from this unit, it is difficult to assess these results.<br />

Although samples BOB-07-05 and BOB-101-14 have been classed as<br />

possibly anomalous, the weak response of the second analysis<br />

(relative to the first analysis) suggest that only limited, if any,<br />

follow-up work is warranted.<br />

- 39 -


l l l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

BEDROCK GEOLOGY<br />

A .l<br />

Introduction<br />

Bedrock chip samples were individually studied under the binocular<br />

microscope and these descriptions are given in Appendix IV, along<br />

with a full listing of the chemistry results. The chemistry results<br />

for ten elements (Ba, Os, Gr, Co, Fe, La, Rb, Se, Th, Na) were used<br />

together with the descriptions to subdivide the bedrock chip samples<br />

into three major groups: metasediments, metagabbros and mafic to<br />

intermediate metavolcanics, and finally, felsic to intermediate<br />

metavolcanics.<br />

The metasedimentary rock descriptions are all very similar, as are<br />

the chemistry results, and this subdivision was quite easy to make.<br />

The other rock descriptions show more variation and the chemistry<br />

results were useful in subdividing them into units. These units are<br />

more heterogeneous and further work will be needed to better<br />

subdivide them.<br />

Finally, a new outcrop was discovered on the property adjacent to one<br />

of the newly constructed drill roads. This outcrop is described in<br />

section A.6, and chemistry results for one sample (JL-40-1) are given<br />

at the end of Appendix IV.<br />

4.2 Metasedimentary Rocks<br />

Bedrock samples taken from the eastern part of the property (eg east<br />

of Nedlog Lake) are mostly very similar. These are quartz-feldsparbiotite<br />

± amphibole ± garnet schists which are interpreted to be<br />

strongly metamorphosed greywackes.<br />

In general, these metasedimentary rocks are fresh and unaltered. A<br />

few samples drilled to a rock flour clay, and this may be due to<br />

preglacial weathering (eg in hole BOB-12, which was protected by the<br />

Missinaibi Sediments unit) or other reasons. Occasional samples<br />

contained disseminated pyrite or pyrite in thin quartz veinlets, but<br />

overall, the samples are very uniform in appearance.<br />

- 40 -


l l l l l l<br />

l l<br />

l l l l l l l l<br />

l l<br />

l<br />

These samples are identified on HAP 10 as biotite schists (BS). A<br />

summary of the chemistry results for 10 elements is given in Table<br />

4-1. Although a few of these samples were difficult to identify<br />

because they drilled to clay, their locations and similar chemistry<br />

strongly suggest that they are the same rock type (see descriptions<br />

in Appendix IV).<br />

Also given in Table 4-1 are average results for two metasediments<br />

taken from outcrops JB-7 and JB-8 and two float boulders taken from<br />

the Burntbush River. The results are comparable, but the bedrock<br />

chip samples carry slightly higher Gr, Co, Fe and Na.<br />

In addition to the abundant greywacke samples, two argillites were<br />

drilled, one within the metasedimentary terrane on the east side of<br />

the property (BOB-127-21), the other within the metavolcanic terrane<br />

west of the Burntbush River (BOB-88-07). These two samples have low<br />

Cs, Gr, Co, Fe and Se contents compared to the greywackes and in some<br />

respects more closely resemble the chemistry of those samples taken<br />

during the summer 1986 program.<br />

Gold content of the metasedimentary rocks is low. Most samples yield<br />

results ^ ppb (detection limit). Eight samples show ^ ppb with<br />

a maximum of 9 ppb in BOB-21-18. The maximum arsenic value in the<br />

east is 10 ppm (BOB-01-10), while BOB-128-17 gave 6.8 ppm. The<br />

argillite sample from the west side (BOB-88-07) gave 11 ppm As. All<br />

other metasedimentary rocks show O ppm As.<br />

4.3 Hetaaabbros and Mafic to Intermediate Metavolcanics<br />

Bedrock samples from twenty-two drill holes (total 26 samples) have<br />

been tentatively identified as metagabbro. It is probable that some<br />

of these rocks are flows, but the size of the bedrock chips makes<br />

identifications difficult. They are composed predominantly of<br />

feldspar and amphibole; biotite and quartz were observed in a few<br />

samples. Most are massive to very weakly foliated and some show a<br />

lineation.<br />

These metagabbros (MG) are also shown on MAP 10 and it can be seen<br />

that their distribution is somewhat erratic. There is good grouping<br />

of metagabbro south and southeast of trench 2, but isolated drill<br />

holes across the metavolcanic terrane have also been labelled<br />

metagabbro. Note that four metagabbros were mapped in outcrop (at<br />

trenches l, 2 and 3 and outcrops JL-17) and that each is associated<br />

with relatively high magnetic signature. Not all of the bedrock chip<br />

samples identified as such fall in high magnetic areas, though.<br />

- 41 -


'<br />

1<br />

1 1111111111111111<br />

Table 4-1 : METASEDIMENTARY ROCKS -<br />

SUMMARY OF ANALYTICAL RESULTS<br />

greywackes metasediments<br />

x 4- an summer '86<br />

(max,min)<br />

x<br />

n = 55 n z 4<br />

argillites<br />

BOB-127 BOB-88<br />

n s 1 n - 1<br />

Ba<br />

(ppm)<br />

Cs<br />

(ppm)<br />

Gr<br />

(ppm)<br />

Co<br />

(ppm)<br />

Fe<br />

(1)<br />

La<br />

(ppm)<br />

Rb<br />

(Ppm)<br />

Se<br />

(ppm)<br />

Th<br />

(ppm)<br />

Ma<br />

W<br />

740 4- 210 620<br />

(1400,420)<br />

4.1 4- 1.6 4.4<br />

(8.1,1.4)<br />

310 4- 62 130<br />

(460,170)<br />

28+5 13<br />

(40,19)<br />

4.9 + 0.7 3.7<br />

(6.7,3.4)<br />

31 + 18 * 20<br />

(150,17)<br />

85 ± 24 83<br />

(140,34)<br />

16 + 2.5 11.4<br />

(22.8,11.0)<br />

6.5 * 2.0 6.3<br />

(14,3.2)<br />

2.9 t 0.5 1.76<br />

(4.26,2,01)<br />

580 630<br />

1.7 1.5<br />

160 160<br />

13 12<br />

3.1 1.9<br />

33 32<br />

71 80<br />

10 6.4<br />

5.4 18,0<br />

2.48 2.41<br />

* if one value of 150 is omitted , the new mean<br />

for La is 29 ± 7 (new maximum value of 57).<br />

- 42 -


l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l<br />

l<br />

In Table 4-2, these "metagabbro" samples are compared with the four<br />

metagabbro outcrops using the same ten elements as in Table 4-1.<br />

In all cases, the chemistry results are comparable. There are some<br />

differences: for example Os values at the sheared metagabbro are<br />

high, and Fe values at trench 3 are low; La and Th results in the<br />

three metagabbros which occur in the northern (high metamorphic)<br />

terrane are also low (trench l and 2, outcrop JL-17). It is also<br />

evident that these ten elements can be used to distinguish these rock<br />

types from the metasediments.<br />

The best gold value obtained from the metagabbros drilled was 14 ppb<br />

from hole BOB-45. It also gave the highest As result (1.6 ppm). All<br />

other gold and arsenic values are less than 10 ppb, and l ppm,<br />

respectively. However, three adjacent holes (BOB-102, 103, 105) just<br />

east of the Burntbush River gave weakly anomalous results of 7 to 8<br />

ppb Au.<br />

The remaining bedrock chip samples have all been identified as<br />

metavolcanic rocks. However, the samples are heterogeneous, i.e.<br />

they are not easily subdivided into units due to their non-uniform<br />

appearance. For this reason we have chosen to subdivide all of the<br />

rocks into two major groups: mafic to intermediate metavolcanics and<br />

felsic to intermediate metavolcanics.<br />

Mafic to intermediate rocks were distinguished from felsic to<br />

intermediate rocks mostly using chemistry results for Fe and Th. Of<br />

course, the descriptions were taken into account, and we found that<br />

high Fe and low Th rocks were nearly always associated with chip<br />

samples identified as intermediate tuffs, while low Fe and high Th<br />

samples were nearly always associated with felsic tuffs.<br />

Table 4-3 summarizes the chemistry results for 24 bedrock chip<br />

samples which have been classed as mafic to intermediate metavolcanic<br />

rocks (HV on HAP 10). When these results are compared with bedrock<br />

chip samples identified as metagabbro, it can be seen that the<br />

results are quite similar. However, on average, the metavolcanics<br />

have slightly lower values for elements associated with mafic<br />

minerals (eg Cr, Co, Fe, Se) and slightly higher values for elements<br />

associated with felsic minerals (eg. Ba, Cs, La, Rb, Th, Ka). This<br />

suggests that in general, we have been able to separate more mafic<br />

rocks from rocks closer to an intermediate composition quite well<br />

using the binocular microscope.<br />

Also shown on Table 4-3 are chemistry results for other metavolcanic<br />

rocks from outcrops within the property.<br />

- 43 -


1 11111111111111111i<br />

t<br />

Table 4-2<br />

"metagabbros"<br />

bedrock chips<br />

-X + on<br />

(max,min)<br />

n ^ 25<br />

Ba 190 ± 80<br />

(ppm) (230^50)<br />

Cs 1.7 * 1.3<br />

(ppm) (5.9,0.5)<br />

Gr 230 + 130<br />

(ppm) (580,72)<br />

Co 50 -f- 24<br />

(ppm) (140,19)<br />

Fe 9.2 + 2.1<br />

W (13.0,6.0)<br />

La 12 + 4<br />

(ppm) (28,5)<br />

Rb 24 + 11<br />

(ppra) (28,5)<br />

Se 29 + 8<br />

(ppm) (49.2,18.0)<br />

Th 1.0 + 0.5<br />

(ppm) (2.3,0.3)<br />

Na 2.0 ± 0.7<br />

a) (3.50,0.64)<br />

: METAGABBROS -<br />

SUMMARY OF ANALYTICAL RESULTS<br />

metagabbro<br />

trench 1<br />

x"<br />

(max,min)<br />

n = 5<br />

100<br />

(190^50)<br />

1.0<br />

(3.0,0.5)<br />

160<br />

(220,64)<br />

33<br />

(37,29)<br />

9.2<br />

(12.0,7.5)<br />

5<br />

(7,2)<br />

18<br />

(39^5)<br />

36<br />

(44.8,30.4)<br />

0.3<br />

(0.4, 0. 2)<br />

2.0<br />

(2.9,1.0)<br />

sheared<br />

metagabbro metagabbro<br />

outcrop<br />

x<br />

JL-17 trench<br />

~~<br />

2<br />

(max, rain)<br />

n = 6<br />

150<br />

(220,54)<br />

1.9<br />

(3.3,0.6)<br />

380<br />

(1100,24)<br />

33<br />

(43,22)<br />

8.4<br />

(11.0,5.5)<br />

4<br />

(5,3)<br />

38<br />

(59,10)<br />

32<br />

(34.7,25.6)<br />

0.3<br />

(0.8, 0. 2)<br />

1.5<br />

(1.9,1.1)<br />

x * "n<br />

(max,min)<br />

n - 50<br />

90 ± 90 *<br />

(610^50)<br />

7.0 ± 14 *<br />

(96.4,0.8)<br />

330 + 110<br />

(560,170)<br />

42+6<br />

(53,27)<br />

9.4 * 0.9<br />

(12.0,6.8)<br />

3 + 1<br />

(7^2)<br />

21 t 29 *<br />

(170^5)<br />

42 + 5<br />

(51.7,29.3)<br />

0.2 + 0.2<br />

(I.l7c0.2)<br />

1.6 + 0.4<br />

(2.36,0.55)<br />

metagabbro<br />

trench 3<br />

x"<br />

(max,min)<br />

n ~ 5<br />

170<br />

(410,86)<br />

1.6<br />

(3. 8, O. 5)<br />

200<br />

(280,73)<br />

29<br />

(39,19)<br />

6.2<br />

(7.3,5.0)<br />

13<br />

(18,9)<br />

31<br />

(88,10)<br />

26<br />

(34.5,17.0)<br />

0.8<br />

(1.5,0.5)<br />

3.3 *<br />

(3.99,1.3)<br />

* if one<br />

for Ba<br />

value of 610 is omitted, the new mean<br />

is 80 i 50 (new maximum value of 260).<br />

* if one<br />

for Cs<br />

value of 96<br />

is 5.2 ± 7<br />

.4 is omitted , the new mean<br />

(new maximum value of 36.0).<br />

* if one<br />

for Rb<br />

* for Na<br />

value of 170 is omitted, the new mean<br />

is 18 ± 20 (new maximum value of 120) .<br />

at trench 3 , n = 4.<br />

- 44 -


1 *<br />

1 Table<br />

1<br />

1<br />

1<br />

4-3 : MAFIC TO INTERMEDIATE METAVOLCANIC ROCKS -<br />

SUMMARY OF ANALYTICAL RESULTS<br />

metavolcanics<br />

bedrock chips<br />

* ± On-l<br />

(max.min)<br />

n = 24<br />

pillowed<br />

basalts<br />

trench 1<br />

x ± "n-1<br />

(max.min)<br />

n o 17<br />

pillowed<br />

andesites<br />

trench 4<br />

x<br />

(max.min)<br />

n - 7<br />

dacitic tuffs<br />

trenches 3, 5<br />

x"<br />

(max.min)<br />

n * 12<br />

1<br />

1<br />

1<br />

1<br />

Ba<br />

(ppm)<br />

Cs<br />

(ppm)<br />

Gr<br />

(ppm)<br />

Co<br />

(ppm)<br />

225 ± 90<br />

(430,120)<br />

2.0 ± 1.0<br />

(5.0,0.8)<br />

210 + 100<br />

(510,57)<br />

36 4- 15<br />

(75,7)<br />

105 4 75<br />

(280^50)<br />

1.1 ± 1.4<br />

(5.8^0.5)<br />

230 * 130<br />

(680,64)<br />

33 * 7<br />

(43,21)<br />

113<br />

(230,67)<br />

2.5<br />

(4.0,1.5)<br />

85<br />

(140,48)<br />

26<br />

(41,20)<br />

330<br />

(690,75)<br />

1.6<br />

(3.7^.5)<br />

20<br />

(58^20)<br />

12<br />

(18,8)<br />

1<br />

Fe<br />

(*)<br />

7.5 ± 1.5<br />

(11.0,5.3)<br />

8.6 ± 1.2<br />

(12.0,6.4)<br />

5.6<br />

(9.1,4.5)<br />

5.4<br />

(12.0,3.0)<br />

1<br />

La<br />

(ppm)<br />

16+6<br />

(31,10)<br />

5 + 2<br />

(9,3)<br />

11<br />

(13,10)<br />

12<br />

(18,9)<br />

1<br />

Rb<br />

(ppm)<br />

37 + 16<br />

(84,17)<br />

18 t 15<br />

(66^5)<br />

15<br />

(23,8)<br />

31<br />

(62,3)<br />

1<br />

1<br />

1<br />

Se<br />

(ppm)<br />

Th<br />

(ppm)<br />

Na<br />

(ppm)<br />

23 + 6<br />

(35.2,11.0)<br />

1.3 * 0.7<br />

(2.8,0.4)<br />

2.3 * 0.8<br />

(4.34,0.58)<br />

37 + 7<br />

(45.3,26.2)<br />

0.3 ± 0.2<br />

(1.07^.2)<br />

1.9 + 0.4<br />

(2.5,1.1)<br />

20<br />

(31.7,16.0)<br />

0.8<br />

(1.1,0.7)<br />

3.0 *<br />

(3.54,2.58)<br />

11<br />

(18.0,7.3)<br />

1.5<br />

(2.2,1.1)<br />

2.1 *<br />

(2.91,0.84)<br />

1<br />

* for Na at<br />

trench 4 , n s 3 ;<br />

at trenches 3, 5 , n s 10<br />

1<br />

1<br />

- 45 -


l l l l<br />

l l l l l l<br />

l l l<br />

l l<br />

l l l<br />

l<br />

A.A<br />

The best gold value obtained from these mafic to intermediate<br />

metavolcanic rocks is 31 ppb in hole BOB-58. This drill hole is<br />

located very close to a northwest trending fault, and just north of<br />

where this fault intersects a second, east-west trending, fault.<br />

Three other samples gave results of 12 to 13 ppb Au (BOB-51-03,<br />

65-05, 67-08). Arsenic values are all O ppm.<br />

Felsic to Intermediate Metavolcanic Rocks<br />

Using descriptions in Appendix IV, and using chemistry results<br />

(summarized in Table 4-4), we have classed all of the remaining<br />

bedrock chip samples as felsic to intermediate metavolcanic rocks.<br />

Five of the drill holes, however, intersected a distinctive reddish<br />

coloured quartzo-feldspathic rock type which can be easily separated<br />

from the other felsic to intermediate rocks. It is described as<br />

porphyritic, carrying rounded to slightly elongate quartz eyes and<br />

generally also carrying feldspar phenocrysts. These samples are<br />

identified as felsic crystal tuffs (XT) on MAP 10, but it may be a<br />

flow rock since the groundmass is very fine grained to aphanitic.<br />

All of these samples were taken along drill section E-E', at the far<br />

western end of the property and are associated with low magnetic<br />

signature. They have very low Gr, Co and Fe values and high Ba and<br />

Na values (see Table 4-4), and are therefore easily distinguished<br />

from the metasedimentary and more mafic metavolcanic rock types using<br />

the chemistry results.<br />

Three additional samples of feldspar crystal tuff were taken from low<br />

magnetic areas at the far western end of the property. These samples<br />

lack the distinctive reddish colour of those described above, but<br />

they too, show very high Na values. However, they probably represent<br />

a different or related subunit of the felsic crystal tuffs described<br />

above since important chemistry differences are apparent (eg lower<br />

Ba, higher Gr, Co, Fe, Se and Th; see Table 4-4).<br />

On MAP 10, these three drill holes are also labelled felsic crystal<br />

tuffs (XT); they can be differentiated from the previous five reddishcoloured<br />

tuffs since they do not fall on section E-E*.<br />

- 46 -


1 111111111111111111 *<br />

Table 4-4 :<br />

FELSIC TO INTERMEDIATE METAVOLCANIC ROCKS -<br />

SUMMARY OF ANALYTICAL RESULTS<br />

felsic crystal<br />

tuffs<br />

TC<br />

(max, rain)<br />

n = 5<br />

feldspar<br />

crystal<br />

tuffs<br />

x<br />

(max,min)<br />

n * 3<br />

felsic tuffs<br />

x"<br />

(max.ndn)<br />

n s 4<br />

int. tuffs<br />

x"<br />

(max,min)<br />

n ~ 4<br />

int. to felsic<br />

flows or tuffs<br />

x<br />

(max.min)<br />

n * 9<br />

BOB-101-16<br />

x<br />

n - l<br />

Ba 1360<br />

(ppm) (1500,1200)<br />

705<br />

(930,330)<br />

1300<br />

(1500,1100)<br />

720<br />

(860,600)<br />

450<br />

(730,220)<br />

1200<br />

Cs 3<br />

(ppm) (4.4,1.7)<br />

1.9<br />

(2.9,1.3)<br />

8.5<br />

(12.0,5.5)<br />

12<br />

(16,6.7)<br />

2.6<br />

(3.9,1.1)<br />

3.6<br />

Gr 130<br />

(ppm) (150,110)<br />

250<br />

(340,190)<br />

310<br />

(440,230)<br />

330<br />

(430,220)<br />

140<br />

(200^20)<br />

84<br />

Co 4<br />

(ppm) (6^5)<br />

14<br />

(17,10)<br />

16<br />

(23,12)<br />

30<br />

(36,23)<br />

15<br />

(24,6)<br />

10<br />

Fe 1.8<br />

W (2.2,1.6)<br />

2.9<br />

(3.2,2.5)<br />

2.9<br />

(3.3,2.2)<br />

4.9<br />

(6.2,3.8)<br />

2.9<br />

(4.6,0.6)<br />

4.5<br />

La 38<br />

(ppm) (48,30)<br />

36<br />

(38,33)<br />

37<br />

(42,29)<br />

30<br />

(39,19)<br />

36<br />

(150,16)<br />

19<br />

Rb 58<br />

(ppra) (63,55)<br />

43<br />

(51,31)<br />

98<br />

(110,84)<br />

118<br />

(160,72)<br />

53<br />

(75,32)<br />

55<br />

Se 3.6<br />

(ppm) (4.6,3.2)<br />

6.9<br />

(8.6,4.6)<br />

9.4<br />

(11.0,7.3)<br />

16<br />

(21.7,14.0)<br />

8.1<br />

(15.0,5.3)<br />

10<br />

Th 3.7<br />

(ppm) (4.0,3.5)<br />

5.1<br />

(5.6,4.7)<br />

5.8<br />

(6.7,4.7)<br />

5.7<br />

(7.6,2.7)<br />

3.5<br />

(5.3,1.7)<br />

2.8<br />

Na 4.3<br />

W (5.15,3.68)<br />

4.3<br />

(4.52,4.11)<br />

1.9<br />

(2.62,0.85)<br />

1.4<br />

(2.41,0.38)<br />

2.7<br />

(4.34,1.0)<br />

0.64<br />

- 47 -


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All of the remaining bedrock chip samples are classed simply as<br />

felsic to intermediate metavolcanics (FV), on MAP 10. These have been<br />

subdivided in Table 4-4 to show that their chemistry is not uniform.<br />

However, they can all be easily distinguished from the metasedimentary<br />

and more mafic metavolcanic rock types.<br />

For example, three drill holes along section E-E' are classed as<br />

felsic tuffs in Table 4-4 (samples BOB-77-03, 77-04, 82-13, 85-10).<br />

Their location and descriptions suggest that they are similar to the<br />

reddish-coloured felsic crystal tuffs but they are greenish coloured<br />

and have low Na values (along with Co, Gr and Fe values more<br />

resembling the feldspar crystal tuffs north of section E-E').<br />

The four remaining samples from profile E-E' are classed (on Table<br />

4-4) as intermediate tuffs. They show higher Co, Fe and Se than the<br />

felsic tuffs.<br />

The other bedrock chip samples which are included in the felsic to<br />

intermediate metavolcanic group are more or less scattered across the<br />

western part of the property. In all cases except one (BOB-90-15),<br />

they are characterized by low magnetic signature. Sample BOB-101-16<br />

may be unique in that it represents the most strongly fractured and<br />

altered bedrock sample taken (although it contains no gold).<br />

Gold values along section E-E' are rather interesting. From felsic<br />

to intermediate rock types, five of twelve drill holes gave 10 ppb or<br />

greater with a maximum value of 28 ppb. Also note that one<br />

metagabbro sample on this section gave 14 ppb Au. Evidence of<br />

shearing was noted in some of these samples, but the bedrock chips<br />

are very small and interpretation of shearing in these samples is<br />

difficult. The aeromagnetic data does not rule out the presence of<br />

an east-west fault close to this drill section.<br />

In the other felsic to intermediate rock samples (those not located<br />

on section E-E'), gold values are all less than 10 ppb. Arsenic<br />

values are O ppm except for hole BOB-53, which gave 10 ppm.<br />

4.5 General Summary of Bedrock Chip Studies<br />

Bedrock samples taken from reverse circulation drill holes support<br />

the main interpretation of the property bedrock geology given in<br />

previous reports. That is, the property can be separated into two<br />

major terranes. To the north, and to the east, the property is<br />

- 48 -


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underlain by a thick sequence of metasediments. These are<br />

principally greywaclces and are strongly metamorphosed. In the<br />

south-central and south-western parts, the bedrock consists of a<br />

complex mixture of metavolcanic flows and tuffs.<br />

The nature of the contact between these two terranes is not yet<br />

known; however, we suspect it is a major east-west break.<br />

Furthermore, we are now beginning to have evidence that the<br />

metavolcanic rocks south of this contact may host multiple, parallel<br />

fault zones.<br />

Our present rock unit subdivisions are adequate only in the<br />

metasedimentary terrane. Further detailing of rock units must be<br />

done in the metavolcanic terrane. Future studies will include<br />

comparison of our rock chips to outcrop samples and diamond drill<br />

core (diamond drilling will be performed starting in February, 1988)<br />

and additional chemistry analyses (eg major element whole rocks) on<br />

selected samples.<br />

4.6 New Outcrop<br />

A previously unreported outcrop was discovered adjacent to a drill<br />

road during the winter 1987 reverse circulation program. It is<br />

located between holes BOB-4O and BOB-50, at about l km due west of<br />

trench 3.<br />

The outcrop is small, only a few metres square. It is composed of<br />

mainly plagioclase and amphibole, similar to the garnetiferous tuffs<br />

at trench 3. A few garnets were observed but they are generally<br />

lacking. The other major difference between this outcrop and the<br />

garnetiferous tuff unit is the abundance of calcite.<br />

Calcite-rich layers are thinly interbedded with the plagioclaseamphibole<br />

layers and the layering is tightly folded at cm scale<br />

(upright, open folds) and nearly horizontal, with fold axes all<br />

plunging gently (~25*) to the east.<br />

A few sterile discordant quartz veins are present.<br />

This outcrop further confirms the abundance of near-horizontal rocks<br />

in the southern metavolcanic terrane.<br />

- 49 -


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5. CONCLUSIONS<br />

5.l Overburden Stratigraphy<br />

Our interpretation of the overburden stratigraphy strongly suggests<br />

that a relatively complex sequence of Wisconsinan glacial deposits is<br />

present in this part of northeastern <strong>Ontario</strong>. The main Wisconsinan<br />

ice sheet appears to have briefly withdrawn and readvanced over the<br />

area, resulting in deposition of two tills.<br />

We conclude that till logged during the field program as "Lower Till"<br />

is in fact equivalent to Matheson Till, and that the younger till is<br />

a late phase also equivalent to Matheson Till (in a regional context).<br />

During the brief interstadial period which separates these two tills,<br />

glaciofluvial and glaciolacustrine sediments were deposited. Since,<br />

in many cases, these are overlain by the younger till, they were also<br />

incorrectly logged during the field program. Thus, most of the<br />

glaciofluvial and glaciolacustrine materials are of late Wisconsinan<br />

age (i.e. Ojibway II unit) and not early Wisconsinan or Sangamon<br />

(i.e. Missinaibi Sediments unit).<br />

It is concluded that pre-Wisconsinan overburden was drilled only in a<br />

restricted area northeast of Blue Lake, where Missinaibi sands and<br />

gravels have been preserved in an area of steep bedrock topography.<br />

In some drill holes, the two Wisconsinan till units are present,<br />

separated by a glaciofluvial or glaciolacustrine marker. In other<br />

holes, where only one till unit was logged in the field, it may be<br />

possible to distinguish which of the two tills is present, or if both<br />

are present. We have not yet fully evaluated our ability to do so,<br />

but As geochemistry results in tills from holes BOB-01 and BOB-02<br />

suggest that there are chemical differences between the two tills.<br />

It is interesting to note that Veillette (1986) has proposed a shift<br />

in ice-flow direction in late Wisconsinan time for the Abitibi-<br />

Timiskaming region. It is possible that this ice-flow direction<br />

change is related to the deposition of the younger till observed in<br />

this area and that the interstadial period recognized in this area is<br />

more a regional than local phenomenon.<br />

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5.2 Overburden Sampling<br />

Gold grain counts and analyses of heavy mineral concentrates from the<br />

overburden samples do not show strong evidence for a mechanical<br />

dispersion train over the southern part of the property.<br />

The best results were taken in an area northeast of Blue Lake, where<br />

protective topography has preserved Missinaibi sands and gravels<br />

which contain significant gold. It is difficult to conclude whether<br />

these results are indicative of bedrock mineralization, or whether<br />

there has been a concentration of gold from pre-existing tills.<br />

We have found that gold grain counts for samples treated at ODH<br />

laboratories in Nepean and Rouyn are not comparable. It is difficult<br />

to assess some of the till samples treated at Rouyn which contain<br />

abundant gold grains (eg 5 to 9 grains) but which give low Au<br />

analyses. Although we conclude that no dispersion train was found,<br />

it is tempting to suggest that some high background samples (eg in<br />

the central part of the property east of the Burntbush River) may<br />

represent the terminal part of a dispersion train which could be<br />

better identified further up-ice.<br />

5.3 Bedrock <strong>Geology</strong><br />

The results of our work on the bedrock chip samples confirm our<br />

earlier interpretations of the bedrock geology. As we have stated in<br />

our previous reports, the property can be subdivided into two main<br />

lithological domains.<br />

The low magnetic area which underlies the northern and eastern part<br />

of the property is considered to be mostly a monotonous, strongly<br />

metamorphosed turbidite sequence. Although outcrops of metabasalt<br />

and metagabbro have been found in this northern domain, none were<br />

intersected in the reverse circulation drill holes.<br />

The high magnetic area which underlies the south-central and south<br />

western parts of the property is composed of a complex metavolcanic<br />

stratigraphy with minor metasedimentary rocks and with interflow<br />

sills and/or intrusive bodies. Metavolcanic rock chips are variable<br />

in appearance and composition and individual rock units are difficult<br />

to map using the drill hole spacing of 400 x 400 m. One exception is<br />

the high-Na, high-Ba reddish coloured quartzo-feldspathic crystal<br />

tuff which is well defined by its low magnetic signature and which<br />

was drilled in five holes near Spade Lake.<br />

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Gold geochemistry of the bedrock chips suggest that the "complex"<br />

southern domain may hold more potential for mineralization than the<br />

"monotonous" northern domain. We suspect that the contact between<br />

the two domains is a shear zone, and therefore a target for gold<br />

mineralization. But, gold values from the southern domain commonly<br />

exceed 10 ppb, whereas this has not yet happened in the northern<br />

domain (except in the sheared metagabbro outcrops interpreted to have<br />

intruded the contact area). Aeromagnetics data and the linear<br />

continuity of anomalous gold results along drill section E-E' suggest<br />

that east-west trending shears are also present within the southern<br />

domain and these targets may be as important as the main sheared<br />

contact zone.<br />

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6. REFERENCE LIST<br />

ASSESSMENT REPORTS (LARDER LAKE MINING DISTRICT)<br />

Ameritex, 1984<br />

COGEMA CANADA LTD, 1987<br />

Geophysical Engineering Ltd, 1976<br />

Averill, S.A. and Thomson, I, 1981, Reverse circulation rotary<br />

drilling and deep overburden geochemical sampling in Master,<br />

Skead, Gauthier and Hearst Townships, District of Timiskaming,<br />

Ont. Geol. Surv. Open File Rept 5335, 276p.<br />

Averill, S.A. and Zitranerman, J.R., 1986, The riddle resolved:<br />

The discovery of the Partridge gold zone using sonic drilling in<br />

glacial overburden at Waddy Lake, Saskatchewan, Can. Geol. J.,<br />

CIMM v.l, p.14-20.<br />

Averill, S.A., 1988, abstract from a paper to be presented at the<br />

Prospecting in Glaciated Terrain symposium in Halifax.<br />

Boissoneau, A.N., 1965, Algoma-Cochrane, Surficial <strong>Geology</strong>, Ont.<br />

Dept. Lands and Forests Map S365, Scale 1:506 880.<br />

Bouchard, M.A., 1986, Pleistocene stratigraphy of northwestern<br />

Abitibi from boreholes and excavations at Selbaie Mine, Quebec,<br />

Geol. Assoc. Can/Mineral. Assoc. Can. Joint Annual Mtg 1986,<br />

Program with Abstracts, p.47.<br />

Clark, T.H., and Steam, C.W., 1968, Geological Evolution of<br />

North America, 2nd ed, The Ronald Press Co, New York, 570p.<br />

Gleeson, C.F. and Sheehan, D.G., 1987, Humus and till geochemistry<br />

over the Doyon, Bousquet and Williams gold deposits, CIM Bull.<br />

v.80, no. 898, p.58-66.<br />

Harron, G.A., Middleton, R.S., Durham, R.B., and Philipp, A, 1987,<br />

Geochemical and geophysical gold exploration in the Timmins<br />

area, <strong>Ontario</strong>: a case history, CIM Bull, v.80, no. 898, p.52-57,<br />

- 53 -


l l l l l l l l l l l l l l l l l<br />

l l<br />

Johns, G.W., 1982, <strong>Geology</strong> of the Burntbush-Detour Lakes area,<br />

District of Cochrane, Ont. Geol. Surv. Kept 199, 82p.<br />

Sauerbrei, J.A., Pattison, E.F., and Averill, S.A., 1987, Till<br />

sampling in the Casa-Berardi gold area, Quebec: a case history<br />

in orientation and discovery, J. Geochem. Expl. v.28, p.297-314.<br />

Shelp, G.S., 1985, The distribution and dispersion of gold in glacial<br />

till associated with gold mineralization in the Canadian Shield,<br />

M.Se thesis, Queen's University, Kingston, Ont., 155p.<br />

Thomson, R., 1936, <strong>Geology</strong> of the Burntbush River area, Ont. Dept.<br />

Mines, Annual Repi v.45, Part 6, p.49-63.<br />

Veillette, J.J., 1986, Former southwesterly ice flows in the<br />

Abitibi-Timiskaming regions: implications for the configuration<br />

of the late Wisconsinan ice sheet, Can. J. Earth Sci., v.23,<br />

p.1724-1741.<br />

- 54 -


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Ref. No. 87-CND-47-04<br />

(Doc. #0076U)<br />

COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

FINAL REPORT - 1987<br />

"REVERSE CIRCULATION DRILLING"<br />

VOLUME 2 of 3<br />

32EiaSW0eM 63.5467 NOSEWORTHY 030<br />

J. Learn<br />

January 1988


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VOLUME<br />

LIST OF APPENDICES<br />

VOLUME 2 of 3;<br />

Appendix I : Drilling Summary and Field Logging Sheets<br />

3 of 3:<br />

Appendix II : ODM Overburden Sample Treatment and Results<br />

Appendix III :<br />

Chimitec HMC Sample Treatment and Results<br />

" Appendix IV : Bedrock Chip Descriptions and Chemistry Results<br />

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APPENDIX I<br />

DRILLING SUMMARY AND FIELD LOGGING SHEETS<br />

- Reverse Circulation Drill Summary<br />

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- Reverse Circulation Drill Hole Logs<br />

By: J. Learn<br />

R. St-Jean<br />

A. Morin<br />

Ref. No. 87-CND-47-04<br />

D. Holmes<br />

(Doc. #0076U) March to July, 1987


1 11<br />

9<br />

1<br />

1<br />

1 1111111111111<br />

HOLE #<br />

DATE<br />

BOB-01<br />

3/3/87<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

7750E<br />

900N<br />

279<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

STRAT 'Y it OF<br />

AND DEPTHS SAMPLES<br />

(0/B)<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

0-3.6<br />

3.6-4.8<br />

4.8-13.0 5<br />

13.0-14.0<br />

14.0-18.6 4<br />

BEDROCK<br />

18.6-20.2<br />

MS, minor sf, cc, q<br />

BOB-02<br />

3/3/87<br />

X<br />

Y<br />

Z<br />

7350E<br />

775N<br />

281<br />

CT<br />

MT<br />

MS<br />

LT<br />

0-3.5<br />

3.5-12.4 5<br />

12.4-18.2<br />

18.2-27.5 5<br />

27.5-29.0<br />

MS, minor sf, cc, q<br />

BOB-03<br />

3*4/3/87<br />

X<br />

Y<br />

Z<br />

6525E<br />

535N<br />

280<br />

CT<br />

MT<br />

0-2.0<br />

2.0-12.0 7<br />

12.0-13.5<br />

MS<br />

BOB-04<br />

4/3/87<br />

X<br />

Y<br />

Z<br />

6925E<br />

645N<br />

278<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-2.0<br />

2.0-13.0<br />

13.0-18.0<br />

18.0-25.6 4<br />

25.6-27.0<br />

MV<br />

BOB-05<br />

4/3/87<br />

X<br />

Y<br />

Z<br />

7460E<br />

1125N<br />

279<br />

CT<br />

Oil<br />

MT<br />

0-6.2<br />

6.2-6.8<br />

6.8-19.5 6<br />

19.5-21.0<br />

MS, minor s f<br />

BOB-06<br />

4/3/87<br />

X<br />

Y<br />

Z<br />

7070E<br />

980N<br />

278<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-2.0<br />

2.0-5.5<br />

5.5-16.5<br />

16.5-20.2 2<br />

20.2-21.7<br />

MS, minor q<br />

BOB-07<br />

4+5/3/87<br />

X<br />

Y<br />

Z<br />

6675E<br />

780N<br />

280<br />

CT<br />

MT<br />

0-2.5<br />

2,5-12.7 7<br />

12.7-14.3<br />

MS, minor q<br />

BOB-08<br />

5/3/87<br />

X<br />

Y<br />

Z<br />

6935E<br />

1350N<br />

275<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-0.5<br />

0.5-11.0<br />

11.0-17.6<br />

17.6-18.5 2<br />

18.5-20.0<br />

MS<br />

BOB-09<br />

5/3/87<br />

X<br />

Y<br />

Z<br />

6550E<br />

1210N<br />

277<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-1.0<br />

1.0-6.5<br />

6.5-7.5<br />

7.5-21.5 10<br />

21.5-23.0<br />

MS


l l l<br />

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HOLE #<br />

DATE<br />

BOB- 10<br />

5/3/87<br />

BOB- li<br />

6/3/87<br />

BOB- 12<br />

6/3/87<br />

BOB- 13<br />

6/3/87<br />

BOB- 14<br />

7/3/87<br />

BOB- 15<br />

7/3/87<br />

BOB-16<br />

7/3/87<br />

BOB- 17<br />

7/3/87<br />

BOB- 18<br />

8/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

6175E<br />

1080N<br />

281<br />

5790E<br />

955N<br />

280<br />

5425E<br />

840N<br />

278<br />

6285E<br />

685N<br />

284<br />

5905E<br />

645N<br />

280<br />

5875E<br />

15 ON<br />

278<br />

5490E<br />

0+20N<br />

280<br />

5130E<br />

110S<br />

287<br />

5525E<br />

505N<br />

278<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

CT<br />

MT<br />

OG<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

CT<br />

Oil<br />

MT<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

# OF<br />

SAMPLES<br />

0-0.6<br />

0.6-1.5<br />

1.5-13.0 4<br />

0-1.0<br />

1.0-7.0<br />

7.0-8.5<br />

8.5-9.6 1<br />

0-1.2<br />

1.2-4.4<br />

4.4-6.8<br />

6.8-24.3 10<br />

24.3-25.1<br />

25.1-37.2 9<br />

0-1.8<br />

1.8-8.5 3<br />

0-1.5<br />

1.5-5.1<br />

5.1-7.7 2<br />

0-2.0<br />

2.0-6.0<br />

6.0-8.0<br />

8.0-9.0 1<br />

0-9.5<br />

9.5-12.0<br />

12.0-21.0 6<br />

0-4.2<br />

4.2-38.1 20<br />

0-1.5<br />

1.5-11.5<br />

11.5-14.7<br />

14.7-22.5 5<br />

BEDROCK<br />

13.0-14.5<br />

MS, MV minor cc, q<br />

9.6-11.1<br />

MS, minor q<br />

37.2-38.7<br />

MV, minor sf, cc<br />

8.5-10.0<br />

MS, minor q<br />

7.7-9.2<br />

MS, minor m. d., q, sf<br />

9.0-10.5<br />

MS, minor q<br />

21.0-22.5<br />

MS, minor q, m. d.<br />

38.1-39.8<br />

MS, m. d. ,<br />

22.5-27.2<br />

MS<br />

minor sf


l l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-19<br />

8/3/87<br />

BOB-20<br />

8/3/87<br />

BOB-21<br />

9/3/87<br />

BOB-22<br />

9/3/87<br />

BOB-23<br />

9+10/3/87<br />

BOB-24<br />

10/3/87<br />

BOB-25<br />

11/3/87<br />

BOB-26<br />

11+12/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

5185E<br />

335N<br />

278<br />

4795E<br />

2 ION<br />

282<br />

4410E<br />

0+95N<br />

283<br />

4360E<br />

355S<br />

281<br />

4755E<br />

245S<br />

288<br />

4030E<br />

0+40S<br />

283<br />

3650E<br />

180S<br />

282<br />

3280E<br />

330S<br />

281<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(coni' d)<br />

STRAT 'Y # OF BEDROCK<br />

AND DEPTHS SAMPLES<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

MT<br />

MS<br />

0-4.4 26.8-28.3<br />

4.4-12.5 MS, minor q<br />

12.5-17.5<br />

17.5-26.8 6<br />

0-1.0 31.8-33.8<br />

1.0-5.5 MS<br />

5.5-7.8<br />

7.8-23.0 10<br />

23.0-31.8 5<br />

0-0.5 43.6-45.1<br />

0.5-3.7 MS, minor m. d.<br />

3.7-15.5 2<br />

15.5-33.5 11<br />

33.5-43.6 4<br />

0-3.0 31.2-32.7<br />

3.0-6.2 MS<br />

6.2-31.2 4<br />

0-0.5 32.6-34.1<br />

0.5-6.5 MS, minor cc<br />

6.5-12.5<br />

12.5-23.0 6<br />

23.0-24.0<br />

24.0-32.6 6<br />

0-0.2 40.8-41.6<br />

0.2-2.9 MS, minor cc<br />

2.9-24.2 14<br />

24.2-39.5 2<br />

39.5-40.8 1<br />

0-0.2 38.0-40.5<br />

0.2-1.7 MV, minor cc, q<br />

1.7-25.8 13<br />

25.8-30.0<br />

30.0-38.0 5<br />

0-0.2 35.8-37.5<br />

0.2-2.0 MS, minor cc, sf, q<br />

2.0-34.4 22<br />

34.4-35.8 1


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-27<br />

12/3/87<br />

BOB-28<br />

13/3/87<br />

BOB-29<br />

14/3/87<br />

BOB-30<br />

14/3/87<br />

BOB-31<br />

15/3/87<br />

BOB-32<br />

16/3/87<br />

BOB-33<br />

16/3/87<br />

BOB- 3 4<br />

17/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

2905E<br />

475S<br />

277<br />

2445E<br />

245S<br />

276<br />

2815E<br />

0+85S<br />

279<br />

3150E<br />

0+20N<br />

281<br />

3550E<br />

185N<br />

282<br />

3925E<br />

335N<br />

284<br />

4290E<br />

470N<br />

283<br />

4665E<br />

590N<br />

281<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(coni 1 d)<br />

STRAT 'Y # OF BEDROCK<br />

AND DEPTHS SAMPLES<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

MS<br />

CT<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

0-3.5 36.9-38.4<br />

3.5-9.5<br />

9.5-16.4<br />

MS, minor q<br />

16.4-36.9 14<br />

0-2.5 27.8-29.3<br />

2.5-8.5 MS<br />

8.5-18.0<br />

18.0-27.8 7<br />

0-1.5 27.0-29.0<br />

1.5-3.0<br />

3.0-4.4<br />

MS, minor q, cc<br />

4.4-27.0 15<br />

0-1.0 45.8-47.3<br />

1.0-1.5 MS, minor q, abund.<br />

1.5-26.0 14 dissem. sf (~1H) py,<br />

26.0-45.8 6 asp<br />

0-1.0 39.3-40.5<br />

1.0-31.8 18 MS, minor ep, q<br />

31.8-34.2 1.5<br />

34.2-39.3 3.5<br />

0-0.1 37.1-38.6<br />

0.1-2.4<br />

2.4-5.0<br />

MS, minor cc, q<br />

5.0-19.8 7<br />

19.8-26.8<br />

26.8-37.1 6<br />

0-0.2 42.1-43.5<br />

0.2-2.4 MS, minor cc, q<br />

2.4-21.5 2<br />

21.5-42.1 12<br />

0-0.3<br />

0.3-1.9 - not reached<br />

1.9-3.0<br />

3.0-13.8 6<br />

13.8-27.8 5<br />

27.8-38.0 6


l l l<br />

l l<br />

l<br />

l l l l l<br />

l l l<br />

l l l l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-35<br />

18/3/87<br />

BOB-36<br />

18/3/87<br />

BOB-37<br />

19/3/87<br />

BOB-38<br />

20/3/87<br />

BOB-39<br />

21/3/87<br />

BOB-40<br />

22/3/87<br />

BOB-41<br />

24/3/87<br />

BOB-42<br />

24/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

5025E<br />

730N<br />

278<br />

2070E<br />

400S<br />

277<br />

1685E<br />

530S<br />

278<br />

1830E<br />

895S<br />

278<br />

2175E<br />

810S<br />

279<br />

835W<br />

1330S<br />

289<br />

5 10W<br />

295S<br />

272<br />

920W<br />

305S<br />

279<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

MT<br />

MS<br />

OG<br />

CT<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

t OF<br />

SAMPLES<br />

0-3.0<br />

3.0-9.6<br />

9.6-13.0<br />

13.0-26.7 9<br />

26.7-29.0<br />

0-0.5<br />

0.5-5.3<br />

5.3-7.2<br />

7.2-24.2 11<br />

24.2-33.5 3<br />

33.5-34.8 1<br />

0-1.6<br />

1.6-3.0<br />

3.0-4.6<br />

4.6-34.0 16<br />

34.0-36.0 1<br />

36.0-45.1 5<br />

0-0.8<br />

0.8-4.0<br />

4.0-4.6<br />

4.6-30.3 13<br />

30.3-38.0 3<br />

0-0.2<br />

0.2-2.5<br />

2.5-34.3 16<br />

34.3-40.2 1<br />

0-1.0<br />

1.0-2.6<br />

0-3.0<br />

3.0-7.8 1<br />

7.8-14.5 4<br />

0-1.2<br />

1.2-2.6 1<br />

2.6-16.3 7<br />

BEDROCK<br />

29.0-30.6<br />

MS, minor cc, mt<br />

34.8-36.5<br />

MS, minor cc, mt, q,<br />

py<br />

45.1-46.0<br />

MV<br />

38.0-39.5<br />

MS, MV minor cc, q, py<br />

40.2-48.0<br />

MV, minor cc, sf<br />

2.6-3.3<br />

MV, minor cc, sf, mt,<br />

q<br />

14.5-16.0<br />

MS, minor cc, q<br />

16.3-17.8<br />

MV, minor q


1 1<br />

9<br />

1 1111111111111111<br />

HOLE #<br />

DATE<br />

CO-ORD<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

# OF<br />

SAMPLES<br />

BEDROCK<br />

BOB-43<br />

24-25/3/87<br />

X<br />

Y<br />

Z<br />

1320W<br />

325S<br />

284<br />

OG<br />

CT<br />

MT<br />

0-0.4<br />

0.4-3.7<br />

3.7-15.2 7<br />

15.2-16.5<br />

MS/MV, minor cc<br />

BOB-44<br />

25/3/87<br />

X<br />

Y<br />

Z<br />

1725W<br />

350S<br />

288<br />

OG<br />

CT<br />

0-0.3<br />

0.3-3.3<br />

3.3-5.0<br />

MV, minor cc, s f<br />

BOB-45<br />

25/3/87<br />

X<br />

Y<br />

Z<br />

2135W<br />

330S<br />

288<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-0.3<br />

0.3-5.5<br />

5.5-7.2<br />

7.2-9.0 1<br />

9.0-10.5<br />

MV, q, minor cc<br />

BOB-46<br />

25/3/87<br />

X<br />

Y<br />

Z<br />

2545W<br />

335S<br />

286<br />

OG<br />

CT<br />

MT<br />

0-0.2<br />

0.2-2.6<br />

2.6-7.0 2<br />

7.0-8.5<br />

MV<br />

BOB-47<br />

25/3/87<br />

X<br />

Y<br />

Z<br />

2950W<br />

345S<br />

285<br />

OG<br />

CT<br />

MT<br />

0-0.2<br />

0.2-2.6<br />

2.6-16.0 6<br />

16.0-17.5<br />

MV, minor sf, cc,<br />

q<br />

BOB-48<br />

26/3/87<br />

X<br />

Y<br />

Z<br />

440W<br />

1220S<br />

284<br />

OG<br />

CT<br />

0-0.2<br />

0.2-1.8<br />

1.8-3.3<br />

MV, minor cc, sf,<br />

q<br />

BOB-49<br />

26/3/87<br />

X<br />

Y<br />

Z<br />

0+70W<br />

1110S<br />

276<br />

OG<br />

CT<br />

MT<br />

0-0.2<br />

0.2-1.2<br />

1.2-9.0 4<br />

9.0-10.5<br />

MV, minor cc, sf,<br />

q<br />

BOB-50<br />

26/3/87<br />

X<br />

Y<br />

Z<br />

mow<br />

1485S<br />

289<br />

OG<br />

CT<br />

0-1.4<br />

1.4-2.0<br />

2.0-3.5<br />

MV, minor cc, sf,<br />

q<br />

BOB-51<br />

26/3/87<br />

X<br />

Y<br />

Z<br />

4 10W<br />

760S<br />

277<br />

OG<br />

CT<br />

MT<br />

0-1.3<br />

1.3-1.9<br />

1.9-5.6 2<br />

5.6-7.5<br />

MV, sf ,<br />

minor q<br />

BOB-52<br />

26/3/87<br />

X<br />

Y<br />

Z<br />

800W<br />

880S<br />

284<br />

OG<br />

CT<br />

Oil<br />

MT<br />

0-1.0<br />

1.0-3.5<br />

3.5-4.5<br />

4.5-7.3 2<br />

7.3-8.8<br />

MV, cc, minor sf


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-53<br />

26/3/87<br />

BOB-54<br />

27/3/87<br />

BOB-55<br />

27/3/87<br />

BOB-56<br />

27/3/87<br />

BOB-57<br />

27/3/87<br />

BOB-58<br />

27/3/87<br />

BOB-59<br />

27-28/3/87<br />

BOB-60<br />

28/3/87<br />

BOB-61<br />

28/3/87<br />

CO-ORD<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

1185W<br />

995S<br />

290<br />

1565W<br />

1095S<br />

292<br />

890W<br />

0+30S<br />

276<br />

1285W<br />

0+20S<br />

282<br />

1695W<br />

04-05N<br />

283<br />

2120W<br />

0+20N<br />

283<br />

2525W<br />

0+30N<br />

283<br />

2950W<br />

0+45N<br />

282<br />

3360W<br />

0+50N<br />

284<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(coni M)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

# OF<br />

SAMPLES<br />

0-0.1<br />

0.1-2.5<br />

2.5-3.7 1<br />

0-2.0<br />

2.0-3.8<br />

3.8-4.4<br />

4.4-9.5 3<br />

0-0.1<br />

0.1-1.9<br />

1.9-3.1<br />

3.1-14.9 7<br />

0-0.2<br />

0.2-2.6<br />

2.6-5.8<br />

5.8-10.8 3<br />

0-1.6<br />

1.6-8.0<br />

8.0-15.2<br />

15.2-18.3 2<br />

0-2.0<br />

2.0-8.0<br />

8.0-14.5<br />

14.5-18.9 3<br />

0-0.7<br />

0.7-2.0<br />

2.0-9.8 5<br />

0-0.4<br />

0.4-3.8<br />

3.8-4.3<br />

4.3-10.7 4<br />

0-1.0<br />

1.0-2.3<br />

2.3-23.5 13<br />

BEDROCK<br />

3.7-5.2<br />

MV, minor sf, q<br />

9.5-11.0<br />

MV, minor s f<br />

14.9-16.3<br />

MV, minor cc<br />

10.8-13.0<br />

MV, minor cc, sf ,<br />

18.3-20.0<br />

MS, minor cc, q<br />

18.9-22.5<br />

MS, MV, minor cc, q<br />

9.8-11.3<br />

MS, minor cc, q<br />

10.7-12.5<br />

MV, q, minor cc<br />

23.5-25.0<br />

MV, minor cc, p<br />

q


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-62<br />

28/3/87<br />

BOB-63<br />

28/3/87<br />

(80)<br />

BOB-64<br />

28/3/87<br />

BOB-65<br />

28/3/87<br />

BOB-66<br />

29/3/87<br />

BOB-67<br />

29/3/87<br />

BOB-68<br />

29/3/87<br />

BOB-69<br />

29/3/87<br />

BOB- 70<br />

29/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

3765W<br />

0+45N<br />

285<br />

4175W<br />

0+55N<br />

286<br />

4585W<br />

0+75N<br />

285<br />

4950W<br />

0+75N<br />

283<br />

5325W<br />

220N<br />

285<br />

5310W<br />

645N<br />

284<br />

6 HOW<br />

605N<br />

288<br />

5775W<br />

620N<br />

285<br />

6525W<br />

625N<br />

292<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cent M)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

OH<br />

OG<br />

CT<br />

on<br />

MT<br />

MS<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

OH<br />

MT<br />

OG<br />

CT<br />

on<br />

MT<br />

# OF<br />

SAMPLES<br />

0-2.0<br />

2.0-6.5<br />

6.5-8.5<br />

8.5-27.5 11<br />

0-1.5<br />

1.5-3,8<br />

3.8-9,0<br />

9.0-10.0 1<br />

0-1.2<br />

1.2-4.6 1<br />

4.6-6.2<br />

6.2-9.8 2<br />

0-1.6<br />

1.6-9.2<br />

9.2-14.2<br />

14.2-21.9 4<br />

0-1.2<br />

1.2-5.0<br />

5.0-11.0 1<br />

0-0.2<br />

0.2-6.0<br />

6.0-13.3 1<br />

13.3-25.6 6<br />

25.6-25.9<br />

0-0.2<br />

0.2-2.0<br />

2.0-2.6<br />

2.6-2.8<br />

0-1.5<br />

1.5-4.0<br />

4.0-8.0<br />

8.0-8.2<br />

0-0.2<br />

0.2-2.5<br />

2.5-2.8<br />

2.8-5.3 2<br />

BEDROCK<br />

27.5-29.0<br />

MV, minor q<br />

10.0-11.5<br />

MV, minor cc<br />

9.8-11.3<br />

MS, minor s f<br />

21.9-23.4<br />

MS, minor q<br />

11.0-12.5<br />

MV, minor cc, sf, q<br />

25.9-27.1<br />

MS, minor cc, q<br />

2.8-4.5<br />

MV, minor sf, q<br />

8.2-10.0<br />

MV, minor sf, q<br />

5.3-6.8<br />

MV, minor s f


l l<br />

l l<br />

l<br />

l<br />

l l<br />

l l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB- 71<br />

29/3/87<br />

BOB- 7 2<br />

29/3/87<br />

BOB- 7 3<br />

29/3/87<br />

BOB- 7 4<br />

29/3/87<br />

BOB- 7 5<br />

29/3/87<br />

BOB- 7 6<br />

29/3/87<br />

BOB- 7 7<br />

29-30/3/87<br />

BOB- 7 8<br />

30/3/87<br />

BOB- 7 9<br />

30/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

6920W<br />

6 ION<br />

293<br />

6970W<br />

285N<br />

293<br />

6560W<br />

270N<br />

292<br />

6145W<br />

245N<br />

290<br />

5 7 SOW<br />

255N<br />

288<br />

5370W<br />

145S<br />

287<br />

5760W<br />

105S<br />

290<br />

6175W<br />

150S<br />

291<br />

6570W<br />

120S<br />

295<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

0-1.5<br />

1.5-2.8<br />

2.8-4.6<br />

4.6-4.7<br />

# OF<br />

SAMPLES<br />

0-1.0<br />

1.0-8.5<br />

8.5-9.5<br />

9.5-15.2 3<br />

0-0.2<br />

0.2-5.0<br />

5.0-7.0<br />

7.0-8.2 1<br />

0-0.2<br />

0.2-8.7<br />

8.7-11.5<br />

11.5-15.7 2<br />

0-1.1<br />

1.1-9.2<br />

9.2-13.0<br />

0-3.7<br />

3.7-6.8<br />

6.8-6.9<br />

0-0.6<br />

0.6-10.6<br />

10.6-14.7<br />

14.7-17.3 2<br />

0-2.6<br />

2.6-8.2<br />

8.2-9.8<br />

9.8-17.9 5<br />

0-0.1<br />

0.1-1.4<br />

1.4-5.0 2<br />

BEDROCK<br />

4.7-6.2<br />

MV, minor sf, cc<br />

15.2-16.5<br />

MV, minor cc, q<br />

8.2-9.7<br />

MV, minor q<br />

15.7-17.2<br />

MV, minor cc, q<br />

13.0-14.5<br />

MV, minor cc, sf, q<br />

6.9-8.4<br />

MV, minor cc, q<br />

17.3-18,8<br />

MV, sf, minor cc, q,<br />

ep<br />

17.9-19.4<br />

MV, minor sf, q, ep<br />

5.0-6.5<br />

MV, minor sf


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-80<br />

30/3/87<br />

BOB-81<br />

30/3/87<br />

BOB-82<br />

30/3/87<br />

BOB-83<br />

30/3/87<br />

BOB-84<br />

30/3/87<br />

BOB-85<br />

31/3/87<br />

BOB-86<br />

31/3/87<br />

BOB-87<br />

31/3/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

6990W<br />

120S<br />

293<br />

4975W<br />

585S<br />

284<br />

4575W<br />

330S<br />

290<br />

4170W<br />

325S<br />

287<br />

3765W<br />

335S<br />

286<br />

3360W<br />

355S<br />

285<br />

4955W<br />

430N<br />

282<br />

4555W<br />

435N<br />

285<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

# OF<br />

SAMPLES<br />

0-3.1<br />

3.1-9.9<br />

9.9-18.0<br />

18.0-21.2 1<br />

0-2.0<br />

2.0-12.5<br />

12.5-26.2<br />

26.2-26.4<br />

0-0.1<br />

0.1-3.6<br />

3.6-4.0<br />

4.0-22.6 12<br />

0-2.8<br />

2.8-6.9<br />

6.9-10.2<br />

10.2-10.8 1<br />

0-3.3<br />

3.3-6.3<br />

6.3-8.5<br />

8.5-20.6 7<br />

0-3.0<br />

3.0-7.4<br />

7.4-11.0<br />

11.0-27.8 9<br />

0-1.3<br />

1.3-8.5<br />

8.5-12.5<br />

12.5-20.0 5<br />

0-2.0<br />

2.0-5.5<br />

5.5-11.0<br />

11.0-18.3 3<br />

BEDROCK<br />

21.2-22.7<br />

MV, minor sf, q<br />

26.4-28.0<br />

MV<br />

22.6-24.1<br />

MV, minor cc, mt, q<br />

10.8-12.3<br />

MV, minor cc, q<br />

20.6-22.5<br />

MV, minor sf, cc, q<br />

27.8-29.1<br />

MV, minor cc, s f<br />

20.0-21.5<br />

MS, minor cc, q<br />

18.3-19.8<br />

MV, minor cc, sf, q


l l l l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l<br />

HOLE 9<br />

DATE<br />

BOB-88<br />

31/3/87<br />

BOB-89<br />

31/3/87<br />

BOB-90<br />

01/4/87<br />

BOB-91<br />

01/4/87<br />

BOB-92<br />

01/4/87<br />

BOB-93<br />

1-^2/4/87<br />

BOB-94<br />

02/4/87<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

CO-ORD<br />

4145W<br />

415N<br />

284<br />

3 7 SOW<br />

390N<br />

285<br />

3330W<br />

360N<br />

286<br />

2915W<br />

330N<br />

284<br />

2515W<br />

305N<br />

284<br />

2105W<br />

290N<br />

283<br />

1700W<br />

265N<br />

283<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y 0 OF BEDROCK<br />

AND DEPTHS SAMPLES<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

CT<br />

MT<br />

MS<br />

LT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

MT<br />

0-1.4 20.6-22.1<br />

1.4-4.0 MS, sf<br />

4.0-8.5<br />

8.5-20.6 6<br />

0-1.3 24.3-25.5<br />

1.3-4.7 MV, minor sf<br />

4.7-9.6<br />

9.6-15.0 3<br />

15.0-16.2 1<br />

16.2-24.3 6<br />

0-1.6 28.3-31.0<br />

1.6-12.3 7 MV, minor cc, q<br />

12.3-13.2<br />

13.2-22.5 5<br />

22.5-28.3 2<br />

0-0.3 20.9-22.4<br />

0.3-5.8 MV<br />

5.8-10.5<br />

10.5-15.3 4<br />

15.3-15.4<br />

15.4-20.9 3<br />

0-1.4 8.1-9.6<br />

1.4-2.9 MV, q, cc, sf<br />

2.9-3.3<br />

3.3-8.1 3<br />

0-1.8 17.7-19.2<br />

1.8-4.3 MV<br />

4.3-6.8<br />

6.8-9.8 2<br />

9.8-11.8<br />

11.8-17.7 4<br />

0-1.4 15.4-16.9<br />

1.4-3.8 MV, minor q, cc<br />

3.8-15.4 7


l l l l l l l l l l l l l l l l l l l<br />

HOLE #<br />

DATE<br />

BOB-95<br />

02/4/87<br />

BOB-96<br />

20/6<br />

(46)<br />

BOB-97<br />

20/6<br />

(49)<br />

BOB-98<br />

21/6<br />

(61)<br />

BOB-99<br />

22/6<br />

(60)<br />

BOB- 100<br />

22/6<br />

(62)<br />

BOB- 101<br />

22/6<br />

(59)<br />

BOB- 102<br />

23/6<br />

(58)<br />

BOB- 103<br />

23/6<br />

(55)<br />

BOB- 104<br />

23-24/6<br />

(54)<br />

CO-ORD<br />

(APPROX)<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

1290W<br />

270N<br />

280<br />

1315E<br />

655S<br />

282<br />

1450E<br />

1090S<br />

282<br />

1060E<br />

1175S<br />

279<br />

675E<br />

1285S<br />

279<br />

930E<br />

790S<br />

281<br />

545E<br />

905S<br />

275<br />

0+65E<br />

570S<br />

277<br />

420E<br />

425S<br />

278<br />

800E<br />

280S<br />

281<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

CT<br />

MT<br />

OG<br />

CT<br />

MT<br />

CT<br />

MT<br />

CT<br />

Oil<br />

MT<br />

OG<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

CT<br />

Oil<br />

MT<br />

CT<br />

MT<br />

OG<br />

CT<br />

MT<br />

MS<br />

LT<br />

0-0.3<br />

0.3-10.0<br />

10.0-15.5<br />

0-1.7<br />

1.7-31.2<br />

0-0.5<br />

0.5-1.5<br />

1.5-24.2<br />

0-2.8<br />

2.8-22.3<br />

0-7.0<br />

7.0-7.2<br />

7.2-10.1<br />

0-0.5<br />

0.5-32.2<br />

0-3.5<br />

3.5-10.0<br />

10.0-11.0<br />

11.0-33.0<br />

0-7.0<br />

7.0-9.5<br />

9.5-37.0<br />

0-1.5<br />

1.5-30.9<br />

0-0.4<br />

0.4-2.3<br />

2.3-35.1<br />

35.1-36.0<br />

36,0-36.8<br />

# OF<br />

SAMPLES<br />

3<br />

2<br />

16<br />

15<br />

12<br />

2<br />

2<br />

18<br />

1<br />

14<br />

13<br />

17<br />

18<br />

1<br />

BEDROCK<br />

15.5-17.0<br />

MV, minor q, cc<br />

31.2-33.2<br />

MV, minor q, cc, sf<br />

24.2-25.7<br />

MV<br />

22.3-24.0<br />

MV, minor cc, s f<br />

10.1-11.7<br />

MV, minor cc, sf, q<br />

32.2-33.7<br />

MV, minor cc, mt<br />

33.0-35.5<br />

MV, v. minor cc,<br />

strongly altered to<br />

rusty colour<br />

37.0-38.0<br />

MV, minor cc<br />

30.9-32.4<br />

MV, minor s f<br />

36.8-38.4<br />

MV, minor sf, q


l l l<br />

l l l<br />

l l<br />

l l l l l l l l<br />

l l<br />

l<br />

HOLE #<br />

DATE<br />

BOB- 105<br />

24/6<br />

(57)<br />

BOB-106<br />

24/6<br />

(56)<br />

BOB-107<br />

25/6<br />

(53)<br />

BOB-108<br />

26/6<br />

(52)<br />

BOB-109<br />

26/6<br />

(51)<br />

BOB- 110<br />

26/6<br />

(50)<br />

BOB- 111<br />

27/6<br />

(119)<br />

BOB- 112<br />

28/6<br />

(121)<br />

CO-ORD<br />

(APPROX)<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

HOW<br />

195S<br />

272<br />

280E<br />

0+60S<br />

282<br />

650E<br />

0+80N<br />

282<br />

1020E<br />

195N<br />

277<br />

1165E<br />

135S<br />

278<br />

1560E<br />

0+05N<br />

276<br />

6630E<br />

1010N<br />

278<br />

6995E<br />

1155N<br />

276<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

MT<br />

CT<br />

MT<br />

06<br />

CT<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

# OF<br />

SAMPLES<br />

0-0.9<br />

0.9-18.5 8<br />

0-1.0<br />

1.0-32.8 18<br />

0-0.5<br />

0.5- 1.5<br />

1.5-26.6 16<br />

26.6-30.5 1<br />

30.5-38.6 5<br />

0-2.5<br />

2.5- 7.6<br />

7.6- 9.0<br />

9.0-28.6 13<br />

0-0.8<br />

0.8-2.0<br />

2.0-31.9 18<br />

31.9-34.5 1<br />

34.5-35.0<br />

0-1.3<br />

1.3-4.1<br />

4.1-6.0 1<br />

6.0-26.2 11<br />

0-1.0<br />

1.0-5.0<br />

5.0-6.7<br />

6.7-23.8 11<br />

0-0.2<br />

0.2-9.5<br />

9.5-14.5<br />

14.5-23.6 6<br />

BEDROCK<br />

18.5-20.0<br />

MV, minor sf, cc, q<br />

not reached<br />

38.6-40.1<br />

MS, minor sf, cc, q<br />

28.6-31.0<br />

MS, minor s f<br />

35.0-37.1<br />

MS, minor sf, q<br />

26.2-28.5<br />

MS, q, v. minor sf<br />

23.8-24.3<br />

MV, v. minor cc, sf<br />

24.3-25.3<br />

MS<br />

23.6-25.1<br />

MS, v. minor q, sf


l l<br />

l l l l<br />

l l l l l<br />

l l<br />

l l l l l<br />

l<br />

HOLE #<br />

DATE<br />

BOB- 113<br />

28/6<br />

(120)<br />

BOB-114<br />

28/6<br />

(122)<br />

BOB- 115<br />

29/6<br />

(124)<br />

BOB- 116<br />

30/6<br />

(123)<br />

BOB-117<br />

30/6<br />

(127)<br />

BOB- 118<br />

1/7<br />

(128)<br />

BOB-119<br />

1/7<br />

(125)<br />

BOB-120<br />

1/7<br />

(126)<br />

CO-ORD<br />

(APPROX)<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

6810E<br />

1080N<br />

277<br />

5600E<br />

890N<br />

278<br />

5525E<br />

1065N<br />

279<br />

5715E<br />

1130N<br />

279<br />

5450E<br />

1255N<br />

279<br />

5260E<br />

1185N<br />

278<br />

5315E<br />

990N<br />

278<br />

5190E<br />

945N<br />

278<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

MT<br />

MS<br />

OG<br />

CT<br />

MT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

f OF<br />

SAMPLES<br />

0-0.2<br />

0.2-1.5<br />

1.5-24.9 12<br />

24.9-25.0<br />

0-2.2<br />

2.2-11.3<br />

11.3-25.0 8<br />

25.0-37.4 5<br />

0-1.4<br />

1.4-6.1<br />

6.1-11.4<br />

11.4-31.1 13<br />

31.1-40.6 4<br />

0-1.1<br />

1.1-7.5<br />

7.5-12.8<br />

12.8-19.7 4<br />

0-1.5<br />

1.5-7.4<br />

7.4-11.9<br />

11.9-19.0 5<br />

0-2.6<br />

2.6-10.8<br />

10.8-12.5<br />

12.5-24.1 7<br />

0-2.4<br />

2.4-8.5<br />

8.5-13.1<br />

13.1-14.8 1<br />

0-3.0<br />

3.0-11.0<br />

11.0-14.7<br />

14.7-17.1 1<br />

BEDROCK<br />

25.0-26.5<br />

MS, v. minor sf, q<br />

37.4-38.9<br />

MS, v. minor sf<br />

40.6-41.8?<br />

Ms, minor sf, q<br />

19.7-21.2<br />

MS, minor sf, q<br />

19.0-20.8<br />

MS, v. minor q<br />

24.1-26.0<br />

MS, minor q<br />

14.8-17.0<br />

MS, minor sf, cc, q<br />

17.1-19.5<br />

MS, minor sf, q


l l<br />

l l<br />

l l<br />

l l<br />

l l l l l l l l l<br />

l<br />

l<br />

HOLE #<br />

DATE<br />

BOB-121<br />

1/7<br />

(129)<br />

BOB-122<br />

2/7<br />

(28)<br />

BOB-123<br />

2/7<br />

(130)<br />

BOB- 124<br />

2-3/7<br />

(29)<br />

BOB-125<br />

3/7<br />

(30)<br />

BOB-125A<br />

3/7<br />

(30)<br />

BOB-126<br />

3-4/7<br />

(31)<br />

BOB-127<br />

4/7<br />

(32)<br />

CO-ORD<br />

(APPROX)<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

5120E<br />

1115N<br />

277<br />

4895E<br />

1110N<br />

278<br />

4980E<br />

920N<br />

278<br />

4480E<br />

1020N<br />

287<br />

4130E<br />

820N<br />

285<br />

4120E<br />

820N<br />

285<br />

3740E<br />

7 ION<br />

280<br />

3340E<br />

570N<br />

282<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

CT<br />

Oil<br />

CT<br />

Oil<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

CT<br />

MT<br />

0-3.2<br />

3.2-10.5<br />

10.5-16.5<br />

16.5-17.5<br />

0-1.0<br />

1.0-4.0<br />

4.0-5.0<br />

5.0-20.4<br />

0-1.1<br />

1.1-8.8<br />

8.8-11.0<br />

11.0-20.0<br />

0-2.0<br />

2.0-12.5<br />

12.5-36.7<br />

36.7-42.0<br />

42.0-45.0<br />

0-1.3<br />

1.3-32.2<br />

0-1.3<br />

1.3-39.8<br />

0-0.2<br />

0.2-5.0<br />

5.0-13.5<br />

13.5-20.8<br />

20.8-31.7<br />

31.7-32.4<br />

0-1.5<br />

1.5-38.5<br />

# OF<br />

SAMPLES<br />

1<br />

9<br />

6<br />

1<br />

13<br />

2<br />

1<br />

3<br />

4<br />

1<br />

20<br />

BEDROCK<br />

17.5-19.5<br />

MS, minor sf, q<br />

20.4-22.5<br />

MS, minor cc, ep,<br />

q, sf<br />

20.0-22.3<br />

MS, minor sf, q<br />

45.0-45.6<br />

MS<br />

32.2-32.5<br />

MS, q, sf<br />

39.8-42.0<br />

MS, q, sf<br />

32.4-34.5<br />

MS<br />

38.5-40.0<br />

MS, v. minor sf


l l<br />

l l l l<br />

l l l<br />

l<br />

l l l<br />

l l l l<br />

l l<br />

HOLE it<br />

DATE<br />

BOB-128<br />

5/7<br />

(33)<br />

BOB-129<br />

5/7<br />

(34)<br />

BOB-130<br />

5/7<br />

(35)<br />

BOB- 131<br />

7/7<br />

(134)<br />

BOB- 13 2<br />

7/7<br />

(133)<br />

BOB-133<br />

7/7<br />

(132)<br />

JL/21.07.87<br />

(doc. #0068U)<br />

CO-ORD<br />

(APPROX)<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

X<br />

Y<br />

Z<br />

2980E<br />

430N<br />

280<br />

2590E<br />

3 ION<br />

278<br />

2240E<br />

135N<br />

276<br />

1500W<br />

4 SON<br />

281<br />

17 05 W<br />

435N<br />

283<br />

1895W<br />

465N<br />

283<br />

REVERSE CIRCULATION<br />

DRILLING SUMMARY<br />

(cont'd)<br />

STRAT 'Y<br />

AND DEPTHS<br />

(0/B)<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

LT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

MS<br />

OG<br />

CT<br />

MT<br />

OG<br />

CT<br />

Oil<br />

MT<br />

f OF<br />

SAMPLES<br />

0-0.8<br />

0.8-2.6<br />

2.6-3.6<br />

3.6-26.4 14<br />

26.4-26.9<br />

26.9-31.2 2<br />

0-2.2<br />

2.2-10.3<br />

10.3-16.2<br />

16.2-28.5 7<br />

28.5-32.3 2<br />

32.3-34.4 1<br />

0-1.2<br />

1.2-5.0<br />

5.0-10.4<br />

10.4-26.9 10<br />

0-0.8<br />

0.8-1.6<br />

1.6-2.1<br />

2.1-15.5 7<br />

15.5-16.2<br />

0-0.5<br />

0.5-2.0<br />

2.0-13.4 7<br />

0-1.5<br />

1.5-5.1<br />

5.1-8.8<br />

8.8-9.9 1<br />

BEDROCK<br />

31.2-33.0<br />

MS, q, minor sf<br />

34.4-36.2<br />

MS, minor s f<br />

26.9-28.5<br />

MS, minor sf, q,<br />

local silicification<br />

16.2-17.5<br />

MV, MS ?<br />

cc, sf, minor ep.<br />

13.4-15.0<br />

MV, q, cc,<br />

minor sf, ep.<br />

9.9-11.2<br />

MV, q, cc,<br />

minor sf, ep.


1<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE3^W> 1937 Sondage No: &&&-DI Localisation: Su^ J<br />

Geologue: bf! , R. 5 j (2.M Sondeur: |J. /^MAjytXT Out LI: CG&&S/-? Metcage: O-cPo.^i<br />

1 Poste (hou re! O<br />

a<br />

1 TOTAL<br />

Sondage: \o;oo -** fi'. JO ; ' ' .<br />

K/fto B*r-^ csggs/f<br />

wevo e IT So6<br />

^ 1 l 1 i1 J h a ' ' 4* ''-t<br />

1 . .. ,, ..... , , . .. -,. ... . .- . .<br />

m Contractant 1 heures) Divers: vtt **to -*x I st itAx *V.30 -* lo'.oo<br />

Deplacement sur le site suivant: 12'. \o ^12.',^<br />

— ECHELLE: 1:100 Page J _ de ^?<br />

m<br />

Profondeur<br />

(m)<br />

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BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE^^v* 195*7 Sondage No: 0c5 3 ~O2. Localisation: JS"if~e- Zx?<br />

n t\. 1 1 n *A i f\ *A/<br />

Geolog ,ue: N-ST Drf R^j Sondeur: /r- Du. re.(r Outil: CB&8&I7 Metra Re: ^0'2- -*^2U<br />

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a Sonda&e:<br />

l2 :1S-tX:VS<br />

1 TOTAL<br />

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JH^ J.987" SondaRe No: 6^6- M 3t Localisation: SlTC 68<br />

Geolog ue: 1?Sh^ f f?.M Sondeur: ^.3)^^11 I-KS Outil: cGkBBIZ.<br />

IPoste (h eures)<br />

— TOTAL<br />

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Hetra Re: 9-3-37. 1<br />

Contractant (heures) Divers:<br />

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m DATE ^5/4*4198^ SondaRe No: fiOfi-^3 Localisation: SJ3 t^<br />

Geolog ue: 1?St-J , RM Sondeur: H.D-u^ff hKf Outil: C668S95 Metre<br />

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DATE iSHe^ol198^ Sondage No: (^O&'^f Localisation: S i G<br />

Geolog ,ue: *}?^f-J PM Sondeur: H,Dx~^.t/ H4S Outil: C& 6G?(*1-<br />

— Poste (lileures)<br />

1<br />

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Contractant (heures)<br />

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Probleraes:<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

oy,lS~- |l;oo<br />

Divers:<br />

Metrage: 9-7 ~ /*/. 7<br />

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8 LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE P S MA^ 1987- Sondage No: 306- tfS' Localisation: Sit ?/<br />

Geolog .ue:1?Sf-J 1?M Sondeur: W.D-uA*f/ fH5 Outil: C8 t,8H8<br />

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BURNTBUSH<br />

RIVER PROJECT<br />

1 LOG SONDAGE. CIRCULATION INVERSE<br />

IDATE P5M-U/W19 8? SondaRe No: G^B'^/k Localisation: S itt 72,<br />

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BURNTBUSH RIVER PROJECT<br />

Contractant ( heures) Divers:<br />

Deplacement sur le site suivant: 2:0O- 8 - l 5~<br />

ECHELLE: 1:100 Page 1 de 7<br />

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Geolog ue: J i- VB Sondeur: R (^ OutLl: rj*,^7/,"^ MetraRe: fi -Z -54, S<br />

IPoste (h leures)<br />

a SondaRe: 6/30 " ^"/^P<br />

— TOTAL<br />

Problemes:<br />

ii-<br />

'- ZOU 3. 3<br />

1 COGE JA C/ iNADA<br />

LIHITEE<br />

(DOc. itO050U)


l l * BURNTBUSH<br />

RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

I<br />

DATE 26/3<br />

'<br />

19 fr? SondaRe No: &O&-44 Localisation: S'f-k )l#<br />

Geologue: J L V6 Sondeur: M C* Outil: C6^7t7<br />

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Poste (h eures)<br />

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— TOTAL<br />

Problemes:<br />

Hetra ge: 54--Z- kS'O<br />

Contractant (heures) Divers:<br />

Deplacement sur le site suivant: ^'i 4-5 - l 0 '' \5<br />

1<br />

ECHELLE: 1:100 Page 1 de J _<br />

1<br />

Profondeur<br />

(m)<br />

1<br />

l l!<br />

l -<br />

l<br />

l<br />

8-<br />

graphique<br />

Log<br />

A 0- .<br />

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^<br />

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o\<br />

01<br />

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03<br />

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~ 0-2 -1-2. Cod-IRAMB Tl LL.J SEMlCA^rt^<br />

— oulck/^ ^o faff St^hl l\t\ni krown f Uy<br />

1.1- ^-o MATMg"50AJ T)tL<br />

AvKtAfcjT<br />

ri rw 5 ^**fvJ si ITV<br />

Co*l T^CT voilr- D^*iy**-A ^(*y^<br />

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fCPO/y) tokp/W, &C/4&/2, (btlMZWll-l)<br />

3-( M'IKC^ bkoiuH cUvey 4i l|<br />

3-5-5,1 /ovo rflni'*! -* IOKA ffl-v^lc<br />

ir^v* *bpv* ck- vt*V tobWy T-( M "^ no<br />

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—- x -t f 1 I'M<br />

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(.<br />

45<br />

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C^fc-POnA/C ^f't^lfif<br />

1 1 ^ ~ /^- ^ /oc**/ rf\\KOY 5 " ^t^ fi ft C i* i f *TtQ***<br />

LIMITEE FO A/ /(?' 5<br />

(Do c. #0050U)


1 *<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

I<br />

DATE 2^/3 J<br />

'<br />

L9 ^ Sondage No: &O&-5O Localisation: ji4e 115<br />

Geologue: JL Vb Sondeur: H D Outil: C6^8?k#<br />

I<br />

M<br />

Poste (heures O<br />

a SondaRe: 10'- lf~ IZ.'45<br />

TOTAL<br />

Problemes: :J~M^' I'l^f cAoitfA H'oo ' 12! 'io<br />

Hetrage: ft - 3- -5<br />

1<br />

IM<br />

1<br />

Contractant ( heures) Divers: KJ&l Bif C6t87k#<br />

ECHELLE: 1:100<br />

Profondeur<br />

i ;<br />

(m)<br />

graphique<br />

Log<br />

A. /V<br />

/\ A<br />

A s\<br />

Echantillon<br />

No<br />

— - --<br />

O\<br />

Deplacement sue le site suivant:<br />

DESCRIPTION<br />

2.0-3.5 6fDfc(XK<br />

— Z. P- 2. 5 lig^ l 1"*/ "f'"^^^'!**^ *iliteoK.4 -twff<br />

|2; 45 -)?!4^<br />

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1<br />

1<br />

1 ,<br />

8-<br />

II-<br />

1 COGE<br />

u c/<br />

HADA<br />

LIMITEE<br />

(DOc. #0050U)


1<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE 2W"? 19 S'? Sondage No: BoB-S\ Localisation: 6\4{, 6b<br />

Geolog ue: JL y ft Sondeur: MO Outil: 666??^^ Hetrane:<br />

M Poste (bcures)<br />

SondaRe:<br />

13 '4 S- )4'.2-f?<br />

. TOTAL<br />

Problemes :<br />

3, 5 -li- o<br />

Contractant ( heures)<br />

Divers:<br />

Deplacement sur le site suivant:<br />

If'.le- I4',30<br />

1<br />

ECHELLE: 1:100<br />

Profondeur<br />

(m)<br />

1 -<br />

graphique<br />

Log<br />

*A<br />

Echantillon<br />

No<br />

DESCRIPTION<br />

O ~ 1. 3 6(S6^AwidS<br />

1.3-1. ^ CotHftMJe TILL<br />

f jOlj t /i/ O.<br />

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v/, mirtof A ifj^**'"^*1 ''^ JwltiAc<br />

in lofally tiliV^cwf B^fTf,<br />

1 COGE *A C/ UADA<br />

LIMITEE<br />

(Do c. #0050U)


1<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE 2.L/3 19 ?1- sondaRe No: RoB~52 Localisation: si-It. ^5<br />

f<br />

Geolog ue: J L V& Sondeur: H h Outil: C6f?7^/?<br />

B Poste (h eures)<br />

<br />

a SondaRe: If, 30~ /t I 3 c?<br />

M TOTAL<br />

Problemes:<br />

Metra Re:<br />

l\.o-\1,8<br />

Contractant { heures)<br />

Divers:<br />

Deplacement sur le site suivant: |t!?O'l^i'^5<br />

ECHELLE: 1:100 Page 1 de /<br />

Profomieur '<br />

(m)<br />

graphique<br />

Log<br />

Echantillon<br />

No<br />

DESCRIPTION<br />

w?*s<br />

if<br />

t^e<br />

HMC<br />

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1 H<br />

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1<br />

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•^ *N - ^L C /*i l/ ftijj A V TT ?C (ilAI CAJ T S<br />

^) * — ' ^J ' ^x ^v ' f? w * f ff *^<br />

- ff^i s*t*v^y silly 1/5^4 3^y ^15^ n^m^<br />

: 7- 3 - S7 . ^ 0g6to|C<br />

T" C**\J|irvQ 'l M ^V"*IA*~^ f* AS)<br />

' ' J 1<br />

I "{^Y ff "rtvi*ily 1 4 *i i K*. i *4 ,<br />

o<br />

o<br />

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n-<br />

1 H<br />

1 13 ~^<br />

1<br />

14-<br />

COGEI 1A C/ HADA<br />

LIMITEE<br />

(DOc. #0050U)


1<br />

,<br />

BURNTBUSH RIVER PROJECT<br />

m<br />

LOG SONDAGE . CIRCULATION INVERSE<br />

I<br />

DATE 2.^/3 19 #? SondaRe No: B06-53 Localisation: S i -^c 44<br />

f<br />

Geologue: JL V6 Sondeur: H b Outii: C.bl,K?6ft Met rage: tf.%'2.5.0<br />

I<br />

Poste (heures )<br />

a SondaRe: )t'45 -12 i' /C<br />

TOTAL<br />

Problemes:<br />

1<br />

Contractant (heures) Divers:<br />

I<br />

Deplacement sue le site suivant: Ifi'K "'#'30<br />

ECHELLE: 1:100 Page 1 de J _<br />

1 q ——————————————————————————<br />

I<br />

3<br />

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^M<br />

1 .-<br />

1 -<br />

1<br />

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graphiqu<br />

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1 -<br />

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1 -<br />

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4<br />

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w<br />

No<br />

01<br />

ol<br />

Btttock<br />

DESCRIPTION<br />

O- O,\ C-RtANldS<br />

';^V:r;;rt)' ^-<br />

— f) l - 2 5 C-o C- tiT&i *J E TI LL<br />

^<br />

2. 5 - 3- ? M^TfjfSox; T/LL<br />

m^iv/Xj ceU/y, tobbly<br />

cl"t^ to**^ pSiTiPv^ ** yOfr&fi-<br />

(tff. Mvy (rfl-l 1-^)<br />

C-ol 0<br />

c^^s<br />

77<br />

o<br />

^.<br />

C/CM<br />

^1 P*<br />

-<br />

^,<br />

sASyi(LJb'''Lt4. ^<br />

tf/yiC (of* bedrock]<br />

fly<br />

n<br />

^<br />

^^<br />

/5.o<br />

/o.o<br />

—<br />

1 -<br />

""^te^^^/.M ^<br />

r .4*1 J, rJb<br />

\/. ri r^, 0 TA ( 1^.^ S 1 1 1 Cd^*X. i TV T T"<br />

1<br />

8-<br />

Q^OK"<br />

1 A fc*l l *\ *1* C ^ ^,**-^ ^* ^ V^* ' ^ J<br />

1 0<br />

1 s-<br />

iftfl n .-V *V * 4,^ * ' P *"*\<br />

kv\ *i KOV yv* STV Co^ T^^ jT'A C- T"** **^ **^ T^ ^^ 5<br />

1 ,<br />

II-<br />

I.<br />

-<br />

r ^o H s. 2<br />

(Doc. ffOOSOU)


1<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE •4<br />

B DATE letfM.***} L95?- Sondage No: QOS~ -5"V Localisation: *b*u 6S.<br />

— Geolog ,ue: n Si^- j n/M<br />

/<br />

Sondeur: H . XiuA^rr. Outtl: fR^8?68 MetraRe: 35, o- 36.0<br />

| Poste ttleures)<br />

a Sondage: *36 ', 3O ~ O&.3O<br />

1 TOTAL<br />

Problemes:<br />

B Contractant (<br />

I<br />

heures) Divers: C^v*^. a~~JV /iA/ (tmLe*. t*~fe~4 . ( itr-faJs./bwiri^t, )<br />

0 'c/<br />

Deplacement sur le site suivant: To 3o0 SS' O8;3O - f/ .00<br />

ECHELLE: 1:100 Page 1 de 1 ~ ~<br />

Profondeur<br />

(m)<br />

1<br />

2-<br />

1 J<br />

1 H<br />

l 'i<br />

l "<br />

l<br />

1<br />

9-<br />

12-<br />

graphique<br />

Log<br />

A<br />

r\<br />

A<br />

A ^<br />

A<br />

/S<br />

A A y<br />

6 '<br />

*<br />

O X ^*<br />

Echantillon<br />

No<br />

M/5<br />

01<br />

05.<br />

03<br />

fJ/S<br />

of<br />

DESCRIPTION<br />

- O. O - 3,0 O fc C, AtJ 1C 5<br />

7Q.O- 3.8 COCHRANE.<br />

T/LL<br />

ft 1 4 Q * fi *fi ~f~- ~,<br />

Ji*. *l\' xv^x-^e. /)^-* ^if 0.1-4-^1* t* /vi-vt UA^<br />

- ff f ' o (To<br />

: i n<br />

A^^y g ^ v, -<br />

i s.S-'i.'i ojiGuj^y IT SCDS.<br />

^i^J ! i fjS^i^'t /i~**^( ^X) ^*X ' ^ Lf*^. l^c t h<br />

j ' f" f<br />

I ij t q . Q ^ p\ fffHZ S&sJ T l L t-<br />

C Lfl.{J\A &Q 1 .3 C^/ c* t At v ^ r^ S/G |? /i. ij<br />

" O ' * "~ O i O Sd-vs. ^*5 C-**-**-^ -Ax^*l XV^. Our~SlA-^y<br />

- fc 8-e.o Cat-Uu - fi^^jcU^ tu*<br />

O^/DX^ . 7 I*'*/<br />

C* i cJ ~~ f5 , 1 0 L-A--*-* A-^1^ /VVA ^i ,/v^n -y<br />

~ 3,3-3,? c*C-tC^ - t-.-teUg "titii.<br />

~QC ii.-N<br />

- J.O - 1 1 -U 01--^<br />

RED^oCK:<br />

Gel 0<br />

#<br />

0<br />

f<br />

;<br />

-<br />

Jo W<br />

^f p^<br />

-<br />

A<br />

A<br />

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fi<br />

fe3<br />

U<br />

2*<br />

^<br />

fl*<br />

l+.o<br />

lo-o<br />

&.0<br />

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w<br />

1<br />

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-— — ^ i&a^ if . —-? ~n**ij, - ,<br />

I.JHITEE<br />

//,<br />

{Tin r .<br />

/*Oosrnn


l<br />

m<br />

^<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE, CIRCULATION INVERSE<br />

m DATE 3?H)uA) 198? Sondage No: QOQ-55 Localisation: Sv"fc Sfi.<br />

Geolog ue: "RSI- J. ^^ Sondeur: H . IX^f/" Outil: CB^Q7(,8 Metrage: 34,*9-5"(p. 3<br />

1 Poste (h leures)<br />

a Sondage: II ;OO - 13 ', ^ 5"<br />

1 TOTAL<br />

Problemes:<br />

B Contractant 1 heures) Divers: \Di~fc Jtn,erZ-t a T lb ,3^^ . — jz^dLcJ*' A#\J.—<br />

I<br />

Deplacement sur le site suivant: To "foOB Sk '. I3',*i5- h'.oo<br />

ECHELLE: 1:100 Page / de S<br />

Profondeur<br />

(m)<br />

1<br />

1 i<br />

2-<br />

1 3-<br />

1 '1<br />

5-<br />

1 H<br />

1<br />

9-<br />

1 l0^<br />

graphique<br />

Log<br />

fcf-<br />

O<br />

A -<br />

- c<br />

•. A<br />

- 0'<br />

*<br />

Echantillon<br />

No<br />

*<br />

0'<br />

o,<br />

03<br />

OH<br />

0^<br />

DESCRIPTION<br />

: O. O- o.i o/^&yQAJ/cTS<br />

1 O.I- |,9 COC /-/f?/0 AJC TILL<br />

V v C J<br />

r 1.9 - 3.1 OJlBuJAV UT SCDS<br />

^ JU^t J*^ t U ^Uj^. ^ ^.<br />

: 3./- x-9. e M AT HE SPA) rt*, t.<br />

-f li ~7 ci /) ' t J *, si* JJ . ^ i " ^<br />

T , 7 —7^ . J Ju* *L/^ ' fy***~*^k /y^-v\ ^^Jt- ^'^^Jl '^^^<br />

st**^* * t* D 1^*1 fi fMS4MV//^^ iLSj<br />

C ^-e*^-~ -^* t t? *^ f -J * ^ f w ' ' -^<br />

: 7.9-9.5" rx^flx.*^^ (3./-?.^<br />

T f .5 - /'- 9 7X^/ r^ *i*^ (3.1-?. *i)<br />

(P-^/A/S<br />

#<br />

O<br />

o<br />

c?<br />

J<br />

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251<br />

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2433<br />

1 3<br />

P^<br />

1<br />

A<br />

/zo<br />

/l?<br />

113<br />

1 COOK<br />

fwx c/<br />

NADA<br />

LIMITEE<br />

(Doc. #0<br />

osou:


l<br />

r<br />

l<br />

l<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

ECHELLE: 1:100 Page P de<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

SHA CANADA LIMITEE<br />

(Doc. 00050U-A)


M -1^1..<br />

~~ ———— ~<br />

1<br />

BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE p? MM 1981 Sondage No: J3PG-S6 Localisation: S it 87<br />

— Geolog ue: TO -J ft/A Sondeur: H . TD^^L^ Outil: C B 68373 Metraae: o- (3. O<br />

g Poste (h leures)<br />

a Sondage: IS 1 o o - It: oo<br />

| TOTAL<br />

Problemes:<br />

1 Contractant ( heures) Divers:<br />

Deplacement sur le site suivant: "To 3^S - S^ ! /^ -' o o - /^ /JO<br />

m ECHELLE: 1:100 I'age ^ de X<br />

Profonrteur<br />

(m)<br />

l -i<br />

2-<br />

1 J<br />

1 '1<br />

graphique<br />

Log<br />

A A.<br />

A \ y<br />

•i ^ '<br />

frV<br />

Echantillon<br />

No<br />

*<br />

DESCRIPTION<br />

; o, 0-0,2. O (Z G fi A^ 1 C S<br />

, r^/^fclf^ T" 1 / J<br />

i a.t-S,B ojiBvxJ^v ir<br />

scbs<br />

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L *--' ' t-* 7 C-^ t ^? /^ * * ^— * ' ^"<br />

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LOG SONDAGE. CIRCULATION INVERSE<br />

DATE StfMa^u 193?- Sondage No: BOQ~(*Z Localisation: ScU<br />

Geoloj ;ue: 1? ^ 1 -J ^ 12 M Sondeur: H-IXu^tff Outil: CO 68833<br />

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BURNTBUSH RIVER PROJECT<br />

LOG SONDAGE. CIRCULATION INVERSE<br />

1 DATE 581 ^La 195f Sondage No: 606 -63 Localisation: St'k 80<br />

Geo log .ue: ffSAJ . jp/f. Sondeur: A/ Dxou-/^ OuLil: C6^eBj3 Metrage: JP.S"- ^Y, O<br />

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LOG SONDAGE. CIRCULATION INVERSE<br />

DATE 2^/3 19 ?f SondaRe No: Soft -^4 Localisation: si-k 71<br />

Geologue: JL V6 Sondeur: Crb Outil: CB&gfll'i<br />

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BURNTBUSH RIVER PROJECT<br />

I<br />

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LOG SONDAGE. CIRCULATION INVERSE<br />

DATE 2 fir/3 J<br />

7<br />

L9 31 SondaRe No: 3c?6-^5" Localisation: Si4e ^^<br />

GeoloRue: J L Vft Sondeur: 6 b Outil: C648&13<br />

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BURNTBUSH<br />

RIVER PROJECT<br />

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IDATE 2*7/3 lg ^7 Sondaae No: fctoB-bb Localisation: S\ 4t- fot?<br />

Geologue: J L Y6 Sondeur: Grb Outil: ce4Sfl9-4 Metraee: 8*.^ -2-1-1<br />

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LOG SONDAGE. CIRCULATION INVERSE<br />

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Geologue: J Sondeur: Outil: C6fe#9"?-4 Metrage: 21 *1-<br />

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1 DATE 2.^/3 19 S? Sondage No: Ro6 - ?4 Localisation: si -k 1 03<br />

Geolog ue: JL V# Sondeur: fab Outil: CR(t ^gS3 Metrage: 4-1-4-47-8<br />

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J DATE 1-2/4 19 #? Sondage No: Qo@ -43 Localisation: s' '4c f 1<br />

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A<br />

A<br />

•A-<br />

^ V.<br />

- i\<br />

V<br />

^ o O O<br />

5 O O<br />

A<br />

:<br />

Echajitillon<br />

01<br />

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i--<br />

No<br />

: 0-1.5 0^^/^U<br />

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DESCRIPTION<br />

"T" *<br />

^-' i -;-'-'V ^^'"C^^'P 1^-3^<br />

•O 1 /- ^ J y\<br />

—— Q O O iJ ^11<br />

— t JLV.^. /.U^" i O^U"0 ^U^- 4 *<br />

~ ^3*C"*vj.J^ \1 /X-1*- '^"^^ ^"^<br />

-. 9 W f 9- O 1 i 1. t ' iu ^^<br />

14-<br />

COGE rtA C/ iNADA LIMITEE ' lO ~<br />

~ ^ J'-J'jJl O Ufc^AJ Vt/^— VJ^/^ /l.,'<br />

— .J<br />

; ^to.t K, ..-',-,^x.v^'. ^ , 4 i/v^- v!^^,,.. X<br />

!O ^ - 1 O c xv K, -i '/i /' .••t<br />

!U.^ | w- /(LCU. vuU\. .'.( JiSjO. '-* V.'vt iO. it.'?<br />

- Cc fK C;<br />

; /I.. cO-.,u,Loc.e( /K-, v'-'^*-"-'<br />

r 10.-- ^-K ^bo-k^) /txA.tUijL- A--' ^^ v^-o<br />

-J -. Y ' v j ) 'J '-' ~" ^ '<br />

J . - 1 . J ' \ i ,<br />

— ,,, Ali-Ct"- .^JXoixTW, TV^, OiO'U,^ /vtA., ^ JUXV<br />

Plo-cfj , ,-v,./....e.., /Uwv^^'i'jtlix. M;o/<br />

fV'^.-:.. . ; O-C-K " ' Hi<br />

1 f*<br />

'<br />

'fi'<br />

1<br />

t \<br />

-'l' w<br />

/\<br />

Page<br />

de<br />

4^;;;: ' ,<br />

C<br />

/Zo<br />

fl*<br />

10.0<br />

(DO c. //O050U)<br />

Jz


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Ref. No. 87-CND-47-04<br />

(Doc. #0076U)<br />

COGEMA CANADA LIMITED<br />

BURNTBUSH RIVER PROJECT<br />

FINAL REPORT - 1987<br />

"REVERSE CIRCULATION DRILLING"<br />

VOLUME 3 of 3<br />

32E12SW00M 63.5467 NOSEWORTHY 040<br />

J. Learn<br />

January 1988


l l<br />

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l<br />

Appendix<br />

l<br />

LIST OF APPENDICES<br />

VOLUME 2 of 3:<br />

I : Drilling Summary and Field Logging Sheets<br />

VOLUME 3 of 3;<br />

Appendix II : ODM Overburden Sample Treatment and Results<br />

Appendix III :<br />

Chimitec HMC Sample Treatment and Results<br />

l<br />

Appendix IV : Bedrock Chip Descriptions and Chemistry Results<br />

l<br />

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l


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l<br />

APPENDIX II<br />

ODM OVERBURDEN SAMPLE TREATMENT AND RESULTS<br />

- Full listing of results from OVERBURDEN DRILLING<br />

MANAGEMENT LTD<br />

- Treatment of Samples<br />

- Laboratory Sample Logs<br />

- Gold Classifications<br />

Note;<br />

SAMPLES BOB-01-01 to BOB-95-05<br />

treated at Nepean Lab<br />

SAMPLES BOB-96-01 to BOB-133-01<br />

treated at Rouyn Lab<br />

Ref. No. 87-CND-47-04<br />

Compiled by: J. Learn<br />

B (Doc. #0076U) January 1988<br />

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APPENDIX II<br />

TREATMENT OF OVERBURDEN SAMPLES<br />

Overburden samples were first sent to OVERBURDEN DRILLING MANAGEMENT Ltd for<br />

preliminary treatment. This laboratory has a specialized capacity to prepare<br />

heavy mineral concentrates, and at the same time check for visible gold grains<br />

in the samples.<br />

A flow chart supplied to us by them is reproduced in Figure 6-1 and is<br />

described below:<br />

1) The sample taken in the field generally weighs 8 to 10 kg.<br />

2) First, ~250 g is removed and stored, as a representative sample of<br />

the original.<br />

3) Next the sample is wet sieved to remove all of the 4-10 mesh (1700 m)<br />

pebble and cobble chips. The relative amounts of metavolcanic and<br />

metasedimentary, granitoid and limestone clasts are recorded, as well<br />

as the dominant clast size, which is estimated by the proportion of<br />

rounded (i.e. worn) surfaces. This part of the sample is then<br />

discarded.<br />

4) The remainder of the sample, generally 7 to 9 kg, is then fed onto a<br />

vibrating table, which is the first step in the preparation of the<br />

heavy mineral concentrate. As the sample feeds down the table, the<br />

heavy minerals are closely watched, and any visible gold grains are<br />

removed and set aside. The light fraction is also observed, and<br />

parameters such as grain size, sorting and colour are noted.<br />

The light fraction is then discarded, and at this point, the sample<br />

weight is greatly reduced (eg to ~200 g).<br />

4A) In the event that 2 or more gold grains are found, or if there are<br />

significant sulfides which might be concealing gold grains, the<br />

sample is subjected to a refined panning process to test for<br />

additional (smaller) gold particles. Any grains found during this<br />

step are also set aside. For most samples, though, this step is<br />

bypassed.<br />

5) The sample then undergoes a heavy liquid separation using methylene<br />

iodide (S.G. = 3.3). This further reduces the sample weight,<br />

generally to ~30 g. The light fraction is stored.


l l l l<br />

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± 250 g STORE<br />

•fi 700y DISCARD<br />

(10 mesh)<br />

Light Fraction^<br />

DISCARD<br />

Light Fraction^<br />

STORE<br />

Magnetic Fraction<br />

STORE<br />

1/4 STORE 4-<br />

-—<br />

(V)<br />

SAMPLE PROCESSING FLOW SHEET<br />

Bulk<br />

Sample<br />

8 - 10 kR<br />

® ^<br />

4 ————— ^q Split 1<br />

Shaking Table<br />

& Gold Grain Count<br />

Heavy Liquid Separation<br />

(Methylene Iodide SG 3.3)<br />

Magnetic<br />

Separation<br />

^ 4- l<br />

T<br />

3/4 Ship to<br />

Analytical Laboratory<br />

Gold Grains<br />

returned<br />

to sample<br />

Panning of<br />

Selected<br />

Samples<br />

Gold Grains<br />

removed<br />

for study


l l l l l l l<br />

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6) The last step in the preparatory process removes magnetic minerals<br />

and drill steel from the sample. This fraction is also stored.<br />

7) Each gold grain detected in steps A and 4A is individually studied<br />

(see below) and then returned to the non-magnetic heavy mineral<br />

fraction (generally ~20 g). This fraction is then split, ~75% is<br />

sent to CHIMITEC Ltee for analysis, and ~25% is stored as a<br />

representative sample.<br />

Individual gold grains are studied in the following manner:<br />

i) they are classed as abraded, irregular or delicate, which is an<br />

effort to estimate the distance of transport;<br />

ii) their dimensions are measured. From this, the estimated gold<br />

concentration due to the grain(s) for the heavy mineral concentrate<br />

is calculated. This helps to establish whether there is any nugget<br />

effect in the CHIMITEC analysis;<br />

CHIMITEC Ltee then receives the heavy mineral concentrate (non-magnetic<br />

fraction) and analyzes for Au and 33 other elements by neutron activation.


1<br />

1 t<br />

11<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED - LABORATORY<br />

ABBREVIATIONS<br />

CLAST :<br />

SIZE OF<br />

Bs<br />

P:<br />

C:<br />

BL:<br />

BK:<br />

y. CLAST<br />

V/S<br />

GR<br />

LS<br />

OT<br />

TR<br />

NA<br />

MATRIX:<br />

S /L!<br />

SO<br />

ST<br />

C Y<br />

COLOR:<br />

B:<br />

BY:<br />

GB:<br />

GN:<br />

GG:<br />

BN:<br />

BK:<br />

OC:<br />

PK:<br />

OE:<br />

DESCRIPTION:<br />

BLD:<br />

BDKs<br />

CLAST:<br />

GRANULES<br />

PEBBLES<br />

COBBLES<br />

BOULDER CHIPS<br />

BEDROCK CHIPS<br />

COMPOSITION<br />

VOLCANICS AND SEDIMENTS<br />

GRANITICS<br />

LIMESTONE<br />

OTHER LITHOLOGIES (REFER TO FOOTNOTES<br />

ONLY TRACE PRESENT<br />

NOT APPLICABLE<br />

SORTED OR UNSORTED<br />

SAND i Y YES FRACTION PRESENT<br />

SILT IN FRACTION NOT PRESENT<br />

CLAY<br />

l<br />

BEIGE<br />

GREY<br />

GREY BEIGE<br />

GREEN<br />

GREY GREEN<br />

BROWN<br />

BLACK<br />

OCHRE<br />

PINK<br />

ORANGE<br />

BOULDER CHIPS<br />

BEDROCK CHIPS<br />

SAMPLE LOG<br />

BELOW)<br />

"<br />

1 F: FINE<br />

! M: MEDIUM<br />

! C: COARSE


l l l<br />

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l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

FOOTNOTES:<br />

A GRITTY CLAY LUMPS PRESENT<br />

B SMOOTH aAY LUMPS PRESENT<br />

C ORGANICS PRESENT<br />

D SAMPLE HIGHLY OXIDIZED


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ABBREVIATIONS<br />

NUMBER OF GRAINS:<br />

THICKNESS:<br />

T: NUMBER FOUND ON SHAKING TABLE<br />

Pi NUMBER FOUND AFTER PANNING<br />

C: CALCULATED THICKNESS OF GRAIN<br />

M: ACTUAL MEASURED THICKNESS OF GRAIN


l<br />

1<br />

V<br />

1<br />

1<br />

1<br />

1 1111111111111<br />

PAGE 1<br />

cobolmar.Hrl<br />

TOTAL i OF SAMPLES IN THIS REPORT = 24<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG.WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

M. I. CONC<br />

CLAST<br />

BOB-87<br />

01-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

02-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

03-01<br />

-02<br />

-03<br />

-04<br />

03-05<br />

TABLE<br />

SPLIT<br />

8.8<br />

7.8<br />

8.3<br />

8.2<br />

4.5<br />

8.9<br />

6.3<br />

7.8<br />

5.3<br />

8.3<br />

9.2<br />

9.8<br />

9.9<br />

4.5<br />

9.9<br />

6.6<br />

7.4<br />

9.5<br />

6.6<br />

9.9<br />

10.0<br />

7.2<br />

9.3<br />

9.5<br />

+10<br />

CHIPS<br />

0.5<br />

0.7<br />

1.0<br />

0.4<br />

0.9<br />

1.0<br />

1.2<br />

0.5<br />

0.5<br />

0.6<br />

0.8<br />

0.8<br />

1.0<br />

0.2<br />

0.1<br />

1.6<br />

1.0<br />

1.2<br />

0.6<br />

0.8<br />

1.0<br />

0.9<br />

1.0<br />

0.6<br />

TABLE<br />

FEED<br />

8.3<br />

7.1<br />

7.3<br />

7.8<br />

3. (S<br />

7.9<br />

7.1<br />

7.3<br />

4.6<br />

7.7<br />

8.4<br />

9.0<br />

8.9<br />

4.3<br />

9.8<br />

7.0<br />

6.4<br />

8.3<br />

6.0<br />

9.1<br />

9.0<br />

6.3<br />

8.3<br />

8.7<br />

TABLE<br />

CONC<br />

208.4<br />

173.7<br />

157.3<br />

131.1<br />

99.1<br />

163.9<br />

160.6<br />

132.4<br />

141.6<br />

160.7<br />

157.9<br />

184.7<br />

190.1<br />

140.9<br />

167.3<br />

160.4<br />

166.4<br />

166.1<br />

196.9<br />

202.2<br />

179.2<br />

136.4<br />

164.2<br />

174.4<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

179.2<br />

147.3<br />

127.0<br />

100.3<br />

80.5<br />

143.6<br />

125.4<br />

106.5<br />

115.7<br />

125.7<br />

120.4<br />

144.8<br />

146.6<br />

123.7<br />

155.0<br />

131.2<br />

144.2<br />

157.8<br />

181.3<br />

174.8<br />

150.8<br />

114.6<br />

134.5<br />

131.0<br />

29.2<br />

26.4<br />

30.3<br />

30.8<br />

18.6<br />

40.3<br />

35.4<br />

25.9<br />

25.9<br />

35.0<br />

37.5<br />

39.9<br />

43.5<br />

17.2<br />

32.3<br />

29.2<br />

22.2<br />

28.3<br />

17.6<br />

27.4<br />

28.4<br />

21.8<br />

29.7<br />

43.4<br />

NW<br />

MAG<br />

16.7<br />

16.7<br />

19.0<br />

19.0<br />

12.6<br />

27.7<br />

22.9<br />

17.5<br />

16.4<br />

22.5<br />

24.6<br />

25.6<br />

26.1<br />

13.1<br />

20.7<br />

19.8<br />

14.3<br />

18.0<br />

11.8<br />

14.7<br />

16.9<br />

12.4<br />

18.0<br />

16.7<br />

NO.<br />

MAG V.G.<br />

10.5<br />

9.7<br />

11.3<br />

11.8<br />

6.0<br />

12.6<br />

12.5<br />

6.4<br />

7.5<br />

12.5<br />

12.9<br />

14.3<br />

17.4<br />

4.1<br />

11.6<br />

9.4<br />

7.9<br />

10.3<br />

5.8<br />

12.7<br />

11.5<br />

9.4<br />

11.7<br />

26.7<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

CALC<br />

PPB<br />

11626<br />

683<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

2539<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

MATRIX<br />

SIZE l S/U SD ST CY COLOR<br />

P<br />

P<br />

P<br />

P<br />

P,C<br />

P, C<br />

P<br />

P,C<br />

P,BK<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

WS GR<br />

60<br />

60<br />

70<br />

75<br />

90<br />

85<br />

85<br />

85<br />

90<br />

69<br />

70<br />

70<br />

80<br />

70<br />

70<br />

80<br />

80<br />

90<br />

60<br />

60<br />

60<br />

35<br />

40<br />

88<br />

LS<br />

40 NA<br />

40 NA<br />

30 NA<br />

25 NA<br />

10 NA<br />

15 NA<br />

14 1<br />

15 NA<br />

10 NA<br />

30 1<br />

30 TR<br />

30 TR<br />

20 TR<br />

30 NA<br />

30 TR<br />

20 NA<br />

20 NA<br />

10 TR<br />

20 TR<br />

40 TR<br />

40 TR<br />

65 NA<br />

60 TR<br />

10 2<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

B<br />

B<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

SD<br />

B<br />

fi<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

CY<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

CLASS<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

04/03/8?


l l<br />

l<br />

PAGE l<br />

cobo2mar.wri<br />

TOTAL t OF SAMPLES IN THIS REPORT a<br />

COGEMA<br />

OVERHJRDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORy SAMPLE LOG<br />

03/24/8?<br />

m<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

NU. :<br />

BOB-87<br />

03-06<br />

-07<br />

04-01<br />

-02<br />

-03<br />

-04<br />

05-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

06-01<br />

-02<br />

07-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

08-01<br />

-02<br />

09-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

10-01<br />

TABLE<br />

Cpl TT<br />

bTL.1 1<br />

8.4<br />

6.7<br />

9.3<br />

8.4<br />

8.8<br />

9.9<br />

9.6<br />

8.7<br />

8.5<br />

9.2<br />

9.8<br />

6.8<br />

9.8<br />

9.6<br />

8.5<br />

8.9<br />

9.7<br />

8.9<br />

9.4<br />

9.4<br />

9.7<br />

8.7<br />

7.6<br />

6.8<br />

9.3<br />

9.0<br />

9.2<br />

7.8<br />

8.9<br />

9.4<br />

9.2<br />

9.4<br />

5.3<br />

8.7<br />

+10<br />

Lnlrb<br />

0.8<br />

0.8<br />

3.0<br />

1.0<br />

0.8<br />

0.8<br />

1.5<br />

2.0<br />

1.2<br />

1.8<br />

1.5<br />

0.8<br />

3.0<br />

2.4<br />

1.6<br />

1.0<br />

1.8<br />

1.0<br />

1.9<br />

2.1<br />

2.1<br />

0.4<br />

0.2<br />

0.7<br />

1.6<br />

1.0<br />

0.6<br />

0.6<br />

1.7<br />

2.0<br />

0.4<br />

1.3<br />

0.3<br />

1.4<br />

TABLE<br />

FEED<br />

7.6<br />

5.9<br />

6.3<br />

7.4<br />

8.0<br />

9.1<br />

8.1<br />

6.7<br />

7.3<br />

7.4<br />

8.3<br />

6.0<br />

6.8<br />

7.2<br />

6.9<br />

7.9<br />

7.9<br />

7.9<br />

7.5<br />

7.3<br />

7.6<br />

8.3<br />

7.4<br />

8.1<br />

7.7<br />

8.0<br />

8.6<br />

7.?<br />

7.2<br />

7.4<br />

8.8<br />

8.1<br />

5.0<br />

7.3<br />

TABLE<br />

/•krtiirv<br />

CONC<br />

162.8<br />

128.9<br />

147.6<br />

149.3<br />

111.6<br />

115.2<br />

97.1<br />

109.4<br />

76.2<br />

110.4<br />

135.3<br />

147.5<br />

325.8<br />

346.2<br />

122.4<br />

116.5<br />

189.4<br />

124.1<br />

152.9<br />

290.2<br />

188.1<br />

98.1<br />

100.3<br />

189.2<br />

150.5<br />

141.9<br />

158.6<br />

128.6<br />

159.6<br />

170.9<br />

123.0<br />

118.6<br />

73.1<br />

126.0<br />

M.I.<br />

LIGHTS<br />

139.9<br />

107.0<br />

115.9<br />

125.6<br />

92.1<br />

94.5<br />

71.5<br />

82.2<br />

51.6<br />

82.2<br />

108.6<br />

130.7<br />

293.5<br />

303.8<br />

96.3<br />

88.1<br />

158.8<br />

101.3<br />

117.9<br />

254.5<br />

160.1<br />

76.0<br />

78.1<br />

157.7<br />

113.6<br />

107.2<br />

127.6<br />

97.9<br />

126.3<br />

139.6<br />

94.9<br />

94.6<br />

56.5<br />

95.7<br />

M.<br />

CONC.<br />

TOTAL<br />

22.9<br />

21.9<br />

31.7<br />

23.7<br />

19.5<br />

20.7<br />

25.6<br />

27.2<br />

24.6<br />

28.2<br />

26.7<br />

16.8<br />

32.3<br />

42.4<br />

26.1<br />

28.4<br />

30.6<br />

22.8<br />

35.0<br />

35.7<br />

28.0<br />

22.1<br />

22.2<br />

31.5<br />

36.9<br />

34.7<br />

31.0<br />

M. 7<br />

33.3<br />

31.3<br />

28.1<br />

24.0<br />

16.6<br />

30.3<br />

I. CONIr<br />

NON<br />

1 Inu<br />

14.3<br />

14.0<br />

18.2<br />

15.3<br />

13.1<br />

13.1<br />

16.2<br />

17.2<br />

16.1<br />

17.0<br />

15.7<br />

10.8<br />

20.5<br />

?7.0<br />

14.6<br />

16.8<br />

17.6<br />

13.5<br />

20.0<br />

21.5<br />

16.3<br />

15.5<br />

16.0<br />

20.1<br />

22.3<br />

21.7<br />

19.2<br />

20.2<br />

22.2<br />

20.0<br />

16.6<br />

13.5<br />

11.0<br />

16.5<br />

rino<br />

8.6<br />

7.9<br />

13.5<br />

8.4<br />

6.4<br />

7.6<br />

9.4<br />

10.0<br />

8.5<br />

11.2<br />

11.0<br />

6.0<br />

11.8<br />

15.4<br />

11.5<br />

11.6<br />

13.0<br />

9.3<br />

15.0<br />

14.2<br />

11.7<br />

6.6<br />

6.2<br />

11.4<br />

14.6<br />

13.0<br />

11.8<br />

10.5<br />

11.1<br />

11.3<br />

11.5<br />

10.5<br />

5.6<br />

13.8<br />

h10.<br />

i't b.<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

2<br />

11<br />

0<br />

2<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

CALC<br />

r re<br />

NA<br />

NA<br />

NA<br />

NA<br />

4296<br />

NA<br />

NA<br />

NA<br />

481<br />

NA<br />

NA<br />

NA<br />

m<br />

2877<br />

198<br />

38<br />

m<br />

580<br />

NA<br />

NA<br />

7362<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

75<br />

NA<br />

NA<br />

NA<br />

NA<br />

SIZE<br />

P<br />

P,BK<br />

P<br />

P<br />

P<br />

P<br />

P,C<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

C<br />

p<br />

c<br />

BK<br />

C<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

p<br />

P<br />

P<br />

1CLAST<br />

iV/SGR<br />

l<br />

80 20<br />

90 10<br />

75 25<br />

84 15<br />

80 20<br />

20 80<br />

75 25<br />

75 25<br />

89 10<br />

90 10<br />

90 10<br />

80 20<br />

70 30<br />

80 20<br />

60 40<br />

60 40<br />

70 30<br />

60 40<br />

60 40<br />

60 40<br />

60 40<br />

55 45<br />

100 NA<br />

70 30<br />

60 40<br />

65 35<br />

70 30<br />

75 25<br />

80 20<br />

80 20<br />

80 20<br />

85 15<br />

80 20<br />

55 40<br />

sssrssssssssrss:<br />

SSSSESCSSSSEZS rssszssrr<br />

LS OT<br />

TR NA<br />

NA NA<br />

TR NA<br />

1 NA<br />

NA A<br />

NA A<br />

NA A<br />

NA NA<br />

1 NA<br />

NA NA<br />

m NA<br />

NA A<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

TR NA<br />

TR NA<br />

TR NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

TR NA<br />

TR NA<br />

NA NA<br />

TR NA<br />

NA NA<br />

TR NA<br />

TR NA<br />

NA NA<br />

NA NA<br />

NA A<br />

5 NA<br />

iS/U SD<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

MATIRIX<br />

ST CY COLOR<br />

SD CY<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL&BDK<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILLfcBDK<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y 6B B TILL<br />

Y Y GB B TILL<br />

Y Y 6B 6Y TILL<br />

Y N GB N TILL<br />

Y Y GB 6Y TILL<br />

Y N B N TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB 68 TILL<br />

Y N GB N TILL<br />

Y Y GB GB TILL<br />

Y Y B B TILL<br />

Y Y B B TILLfcBDK<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y 66 GB TILL<br />

l<br />

l


l<br />

l<br />

l<br />

PAGE l<br />

COB03MAR.WRI<br />

TOTAL # OF SAMPLES IN THIS REPORT 40<br />

COGEMA<br />

OVERBIDDEN DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

04/03/67<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

SAMPLE<br />

NO.<br />

BOB-87<br />

10-02<br />

-03<br />

-04<br />

11-01<br />

12-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-16<br />

-19<br />

13-01<br />

-02<br />

-03<br />

14-01<br />

-02<br />

15-01<br />

16-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

17-01<br />

-02<br />

-03<br />

-04<br />

17-05<br />

fc EIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

TABLE<br />

SPLIT<br />

9.3<br />

8.3<br />

9.6<br />

8.2<br />

9.7<br />

9.0<br />

9.2<br />

8.9<br />

9.1<br />

9.7<br />

8.4<br />

8.8<br />

9.1<br />

8.6<br />

9.1<br />

9.2<br />

9.2<br />

9.4<br />

9.7<br />

9.8<br />

8.9<br />

9.0<br />

6.9<br />

5.8<br />

7.3<br />

7.9<br />

9.4<br />

9.1<br />

8.7<br />

9.3<br />

6.9<br />

8.3<br />

9.1<br />

9.2<br />

9.2<br />

6.3<br />

9.0<br />

8.8<br />

9.2<br />

8.5<br />

+10<br />

CHIPS<br />

1.2<br />

0.6<br />

1.0<br />

0.7<br />

0.8<br />

0.5<br />

0.6<br />

0.7<br />

0.1<br />

0.6<br />

1.0<br />

0.5<br />

1.1<br />

0.6<br />

0.4<br />

1.5<br />

1.2<br />

2.2<br />

2.1<br />

.0<br />

.0<br />

0.9<br />

.2<br />

.2<br />

.8<br />

.0<br />

.7<br />

1.6<br />

1.0<br />

0.5<br />

0.5<br />

0.6<br />

0.3<br />

0.4<br />

0.8<br />

0.4<br />

0.5<br />

0.5<br />

0.4<br />

0.3<br />

TABLE<br />

FEED<br />

8.1<br />

7.7<br />

8.6<br />

7.5<br />

8.9<br />

8.5<br />

6.6<br />

8.2<br />

9.0<br />

9.1<br />

7.4<br />

8.3<br />

8.0<br />

8.0<br />

8.7<br />

7.7<br />

8.0<br />

7.2<br />

7.6<br />

6.8<br />

7.9<br />

8.1<br />

7.7<br />

4.6<br />

5.5<br />

6.9<br />

7.7<br />

7.5<br />

7.7<br />

8.8<br />

6.4<br />

7.7<br />

8.6<br />

6.6<br />

8.4<br />

5.9<br />

8.5<br />

6.3<br />

8.8<br />

6.2<br />

TABLE<br />

CONC<br />

81.7<br />

106.6<br />

103.7<br />

99.1<br />

122.6<br />

119.0<br />

102.2<br />

104.1<br />

113.8<br />

185.4<br />

117.6<br />

166.6<br />

243.6<br />

135.8<br />

158.2<br />

289.3<br />

203.9<br />

227.9<br />

269.4<br />

227.5<br />

260.0<br />

165.2<br />

235.2<br />

105.2<br />

150.8<br />

149.1<br />

122.8<br />

126.3<br />

178.7<br />

228.2<br />

194.1<br />

192.5<br />

188.6<br />

208.9<br />

200.1<br />

173.5<br />

193.8<br />

203.7<br />

214.8<br />

208.5<br />

M. I. CONC<br />

M.I. CONC. NON<br />

LIGHTS TOTAL MAG<br />

54.2<br />

82.5<br />

76.8<br />

73.9<br />

90.1<br />

87.9<br />

67.2<br />

74.4<br />

89.3<br />

161.6<br />

93.2<br />

131.5<br />

193.4<br />

102.9<br />

124.1<br />

235.8<br />

166.6<br />

190.2<br />

168.0<br />

149.1<br />

225.4<br />

144.2<br />

228.0<br />

61.0<br />

124.8<br />

123.7<br />

93.5<br />

97.0<br />

146.5<br />

189.8<br />

167.4<br />

161.9<br />

158.7<br />

172.0<br />

168.9<br />

152.9<br />

163.4<br />

175.0<br />

165.9<br />

175.4<br />

27.5 17.1<br />

26.3 16.3<br />

26.9 16.9<br />

25.2 15.6<br />

32.5 20.5<br />

31.1 19.8<br />

35.0 22.9<br />

29.7 20.2<br />

24.5 15.8<br />

23.8 13.8<br />

24.4 15.8<br />

35.3 23.8<br />

50.2 29.4<br />

32.9 21.9<br />

34.1 24.1<br />

53.5 30.4<br />

37.3 23.2<br />

37.7 21.6<br />

EI. 4 45.0<br />

76.4 46.3<br />

34.6 18.4<br />

21.0 14.5<br />

7.2 4.8<br />

24.2 13.7<br />

26.0 13.9<br />

25.4 15.2<br />

29.3 17.4<br />

29.3 18.0<br />

30.2 20.2<br />

38.4 25.4<br />

26.7 17.2<br />

30.6 19.1<br />

29.9 19.0<br />

36.9 22.1<br />

31.2 20.8<br />

20.6 12.3<br />

30.4 19.4<br />

26.7 18.4<br />

28.9 18.6<br />

33.1 22.5<br />

NO.<br />

MAG V.G.<br />

10.4<br />

10.0<br />

10.0<br />

9.6<br />

12.0<br />

11.3<br />

12.1<br />

9.5<br />

B.7<br />

10.0<br />

8.6<br />

11.5<br />

20.8<br />

11.0<br />

10.0<br />

23.1<br />

14.1<br />

15.9<br />

36.4<br />

32.1<br />

16.2<br />

6.5<br />

2.4<br />

10.5<br />

12.1<br />

10.2<br />

11.9<br />

11.3<br />

10.0<br />

13.0<br />

9.5<br />

11.5<br />

10.9<br />

14.8<br />

10.4<br />

8.3<br />

11.0<br />

10.3<br />

10.3<br />

10.6<br />

0<br />

0<br />

1<br />

0<br />

7<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

8<br />

0<br />

2<br />

19<br />

3<br />

1<br />

7<br />

13<br />

1<br />

0<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

CLAST<br />

MATI<br />

CALC SIZE X S/U SD<br />

ppg srrsrssrrsrrsrs<br />

V/S GR<br />

LS OT<br />

NA P 45 50 5 NA U Y<br />

NA P 40 50 10 NA U Y<br />

171 P 30 60 10 NA U Y<br />

NA P 60 40 TR A U Y<br />

1373 P 65 35 TR NA U Y<br />

NA P 50 50 NA NA U Y<br />

498 P 50 50 TR NA U Y<br />

NA C 55 45 TR NA U Y<br />

NA C 55 45 TR NA U Y<br />

NAC 7030NANAUY<br />

NA C,BL 70 30 TR NA U Y<br />

NAP,BLBO 20 TR NA U Y<br />

3260 C 55 45 TR A U Y<br />

NA P 60 40 TR A U Y<br />

23 C 80 20 TR NA U Y<br />

7568 P,BL 55 45 TR NA U Y<br />

2117 P,BL 50 50 TR NA U Y<br />

523 P 55 45 TR NA U Y<br />

489 P 55 45 TR NA U Y<br />

593 P 60 40 TR NA U Y<br />

82 P 30 70 TR NA U Y<br />

NA P 30 69 I NA U Y<br />

NA P 40 59 1 NA U Y<br />

832 P 40 60 NA NA U Y<br />

557 P 45 55 TR NA U Y<br />

NAP.BK69 25 1 NA U Y<br />

NA P 45 54 1 NA U Y<br />

NA P 40 59 1 NA U Y<br />

NA P 65 35 TR NA U Y<br />

NA P 30 70 NA NA U Y<br />

NA P 35 64 1 NA U Y<br />

NA P 70 30 TR NA U Y<br />

NA P 60 40 NA ' A U Y<br />

NA P 80 20 NA A U Y<br />

NA P 90 10 NA NA U Y<br />

NA P 60 40 NA NA U Y<br />

NA P 60 40 NA NA U Y<br />

NA P 70 30 TR NA U Y<br />

NA P 70 30 TR NA U Y<br />

NA P 70 30 NA NA U Y<br />

srsrzzrrzrrSES ssssssssss<br />

m<br />

ST CY COLOR<br />

ssssss<br />

SD CY<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y N B<br />

Y N B<br />

Y N B<br />

Y N B<br />

Y N B<br />

Y N B<br />

Y Y B<br />

Y N B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y<br />

Y<br />

Y B<br />

Y GB<br />

Y Y 6Y<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

CLASS<br />

6B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

66 TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL&BLD<br />

B<br />

NA TILL<br />

NA TILL<br />

NA TILL<br />

NA TILL<br />

NA TILL<br />

NA TILL<br />

TILL&BLD<br />

B TILL<br />

NA TILL<br />

6B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

6Y TILL<br />

GY TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

6 TILL<br />

B TILL


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE i<br />

COB04MAR.WRI<br />

TOTAL t OF SAMPLES IN THIS REPORT * 41<br />

COGEHA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

04/<br />

DESCRIPTION<br />

CLASS<br />

NU. :<br />

BOB-87<br />

17-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

18-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

19-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

20-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

20-15<br />

TABLE<br />

SPLIT<br />

8.3<br />

9.2<br />

8.9<br />

8.9<br />

6.5<br />

9.2<br />

6.0<br />

9.6<br />

9.5<br />

7.8<br />

7.6<br />

9.8<br />

9.7<br />

8.6<br />

9.2<br />

9.7<br />

6.0<br />

8.6<br />

7.1<br />

9.0<br />

6.2<br />

9.4<br />

9.0<br />

9.6<br />

9.2<br />

9.0<br />

9.0<br />

9.5<br />

9.4<br />

9.1<br />

9,5<br />

7.5<br />

9.0<br />

8.6<br />

9.0<br />

9.0<br />

9.0<br />

8.7<br />

9.4<br />

6.9<br />

8.7<br />

+10<br />

CHIPS<br />

0.3<br />

0.3<br />

0.9<br />

0.4<br />

0.5<br />

0.5<br />

0.5<br />

0.6<br />

1.5<br />

1.2<br />

0.6<br />

0.6<br />

0.8<br />

0.2<br />

0.8<br />

1.4<br />

0.5<br />

0.8<br />

1.2<br />

1.4<br />

1.2<br />

1.3<br />

1.4<br />

1.7<br />

0.4<br />

0.6<br />

2.2<br />

3.0<br />

2.0<br />

2.2<br />

3.0<br />

0.4<br />

0.8<br />

1.0<br />

0.5<br />

0.8<br />

2.4<br />

1.5<br />

1.1<br />

1.9<br />

1.4<br />

TABLE<br />

FEED<br />

8.0<br />

8.9<br />

8.0<br />

8.5<br />

6.0<br />

8.7<br />

7.5<br />

9.0<br />

8.0<br />

6.6<br />

6.6<br />

9.0<br />

8.9<br />

8.4<br />

6.4<br />

8.3<br />

5.5<br />

7.8<br />

5.9<br />

7.6<br />

7.0<br />

8.1<br />

7.6<br />

7.9<br />

6.6<br />

6.4<br />

6.6<br />

6.5<br />

7.4<br />

6.9<br />

6.5<br />

7.1<br />

8.2<br />

7.6<br />

8.5<br />

8.2<br />

6.6<br />

7.2<br />

8.3<br />

7.0<br />

7.3<br />

TABLE<br />

CONC<br />

201.5<br />

169.4<br />

120.1<br />

123.5<br />

122.1<br />

147.0<br />

107.4<br />

108.2<br />

96.6<br />

123.6<br />

129.4<br />

111.4<br />

131.3<br />

100.6<br />

130.4<br />

146.6<br />

137.9<br />

104.5<br />

100.4<br />

133.3<br />

115.2<br />

112.0<br />

96.2<br />

96.2<br />

62.4<br />

207.1<br />

302.5<br />

220.6<br />

233.9<br />

255.1<br />

259.5<br />

206.1<br />

215.6<br />

147.0<br />

176.6<br />

156.3<br />

213.0<br />

154.8<br />

182.9<br />

168.1<br />

197.3<br />

M. l<br />

M.I.<br />

CONC.<br />

LIGHTS TOTAL<br />

171.0<br />

119.9<br />

90.6<br />

93.6<br />

96.2<br />

117.9<br />

63.6<br />

80.5<br />

65.7<br />

76.0<br />

103.3<br />

90.0<br />

104.1<br />

74.3<br />

110.1<br />

123.4<br />

108.6<br />

80.0<br />

74.2<br />

107.7<br />

94.6<br />

85.3<br />

71.6<br />

68.4<br />

34.0<br />

181.7<br />

260.0<br />

186.6<br />

200.3<br />

217.7<br />

211.6<br />

161.0<br />

173.5<br />

120.5<br />

145.7<br />

133.8<br />

165.0<br />

125.8<br />

152.1<br />

138.2<br />

162.3<br />

30.5<br />

49.5<br />

29.5<br />

29.9<br />

25.9<br />

29.1<br />

23.8<br />

27.7<br />

31.1<br />

47.6<br />

26.1<br />

21.4<br />

27.2<br />

26.3<br />

20.3<br />

25.2<br />

29.3<br />

24.5<br />

26.2.<br />

25.6<br />

20.6<br />

26.7<br />

24.6<br />

27.6<br />

28.4<br />

25.4<br />

42.5<br />

34.0<br />

33.6<br />

37.4<br />

47.9<br />

45.1<br />

42.3<br />

26.5<br />

30.9<br />

22.5<br />

26.0<br />

29.0<br />

30.8<br />

29.9<br />

35.0<br />

1. CONC<br />

NON<br />

MAS<br />

19.0<br />

28.1<br />

16.6<br />

19.1<br />

16.3<br />

18.0<br />

14.6<br />

16.7<br />

16.6<br />

21.9<br />

16.0<br />

13.0<br />

17.2<br />

10.7<br />

14.1<br />

15.2<br />

12.2<br />

15.6<br />

15.7<br />

15.7<br />

12.6<br />

16.5<br />

16.0<br />

17.7<br />

19.3<br />

16.2<br />

26.2<br />

22.1<br />

21.3<br />

22.0<br />

29.9<br />

27.6<br />

25.6<br />

17.1<br />

19.9<br />

14.6<br />

15.9<br />

16.7<br />

18.5<br />

19.8<br />

9.6<br />

NO.<br />

MAG V.G.<br />

11.5<br />

21.4<br />

10.9<br />

10.8<br />

9.6<br />

11.1<br />

9.0<br />

11.0<br />

14.3<br />

25.7<br />

10.1<br />

6.4<br />

10.0<br />

15.6<br />

6.2<br />

10.0<br />

17.1<br />

6.7<br />

10.5<br />

9.9<br />

7.8<br />

10.2<br />

8.6<br />

10.1<br />

9.1<br />

9.2<br />

16.3<br />

11.9<br />

12.3<br />

15.4<br />

18.0<br />

17.5<br />

16.7<br />

9.4<br />

11.0<br />

7.9<br />

12.1<br />

12.3<br />

12.3<br />

10.1<br />

25.4<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

3<br />

1<br />

1<br />

0 1 0<br />

0<br />

0 11 0 1 0 1 0<br />

0<br />

0<br />

0<br />

0 1i1 0<br />

0<br />

0<br />

0 1 0<br />

0<br />

0<br />

CALC<br />

PPB<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

22<br />

NA<br />

NA<br />

214<br />

123<br />

358<br />

NA<br />

190<br />

NA<br />

NA<br />

NA<br />

135<br />

166<br />

NA<br />

1001<br />

NA<br />

150<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

50<br />

54<br />

1424<br />

m<br />

NA<br />

NA<br />

NA<br />

90<br />

NA<br />

NA<br />

NA<br />

CLAST<br />

SIZE<br />

:<br />

\<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P,BL<br />

P<br />

p P<br />

P,BL<br />

C<br />

P<br />

C<br />

P<br />

P<br />

P P C<br />

P<br />

P<br />

P<br />

P<br />

p<br />

C P P<br />

C<br />

C<br />

C<br />

c cpcccpp G<br />

P<br />

i<br />

'/S GR<br />

85<br />

85<br />

75<br />

80<br />

75<br />

70<br />

70<br />

30<br />

50<br />

40<br />

25<br />

35<br />

40<br />

65<br />

40<br />

30<br />

30<br />

40<br />

30<br />

50<br />

39<br />

55<br />

60<br />

60<br />

65<br />

55<br />

60<br />

60<br />

55<br />

45<br />

58<br />

60<br />

60<br />

68<br />

80<br />

65<br />

55<br />

35<br />

49<br />

50<br />

50<br />

15<br />

15<br />

25<br />

20<br />

25<br />

30<br />

30<br />

70<br />

50<br />

60<br />

75<br />

25<br />

59<br />

35<br />

60<br />

70<br />

70<br />

60<br />

70<br />

50<br />

60<br />

45<br />

40<br />

40<br />

35<br />

40<br />

40<br />

40<br />

45<br />

55<br />

40<br />

40<br />

40<br />

30<br />

20<br />

35<br />

45<br />

65<br />

50<br />

50<br />

50<br />

sssssssssssssssss—ssssssssss ""~<br />

MATRIX<br />

LS<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

40<br />

1<br />

TR<br />

TR<br />

TR<br />

NA<br />

TR<br />

NA<br />

NA<br />

1<br />

NA<br />

NA<br />

TR<br />

NA<br />

5<br />

TR<br />

TR<br />

TR<br />

TR<br />

2<br />

NA<br />

TR<br />

2<br />

TR<br />

TR<br />

TR<br />

TR<br />

1<br />

TR<br />

TR<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

S/U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

SD<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

ST<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

CY<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

COLOR<br />

SD<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

66<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

CY<br />

B<br />

68<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

6B<br />

GB<br />

GB<br />

6B<br />

B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

6<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B B<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE i<br />

COB01APR.WRI<br />

TOTAL t OF SAMPLES IN THIS REPORT = 40<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

04<br />

SAMPLE WEIGHT (KG.HET) WEIGHT (GRAMS DRV) AU DESCRIPTION CLASS<br />

IU. ;<br />

OB-87<br />

21-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

22-01<br />

-02<br />

-03<br />

-04<br />

23-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

24-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

24-07<br />

TABLE<br />

SPLIT<br />

7.5<br />

8.5<br />

6.6<br />

6.4<br />

6.6<br />

9.0<br />

7.2<br />

9.0<br />

10.2<br />

9.4<br />

9.4<br />

9.7<br />

9.2<br />

6.9<br />

9.6<br />

9.3<br />

9.2<br />

8.9<br />

9.0<br />

8.9<br />

8.6<br />

9.1<br />

9.1<br />

9.3<br />

9.1<br />

8. B<br />

7.6<br />

9.3<br />

7.9<br />

8.5<br />

8.2<br />

8.8<br />

9.0<br />

8.2<br />

9.1<br />

6.9<br />

8.5<br />

8.8<br />

9.5<br />

8.8<br />

•HO<br />

CHIPS<br />

0.0<br />

0.0<br />

0.9<br />

0.5<br />

0.6<br />

1.2<br />

0.9<br />

1.0<br />

3.3<br />

1.2<br />

1.2<br />

1.4<br />

2.0<br />

0.1<br />

2.2<br />

1.6<br />

0.3<br />

0.0<br />

0.0<br />

0.5<br />

0.1<br />

1.0<br />

1.0<br />

0.8<br />

0.9<br />

0.7<br />

0.2<br />

1.2<br />

0.9<br />

1.0<br />

0.9<br />

0.8<br />

1.6<br />

1.5<br />

1.0<br />

0.7<br />

0.4<br />

0.9<br />

0.8<br />

1.1<br />

TABLE<br />

FEED<br />

7.5<br />

8.5<br />

5.9<br />

5.9<br />

6.0<br />

7.8<br />

6.3<br />

8.0<br />

6.9<br />

8.2<br />

8.2<br />

8.3<br />

7.2<br />

8.8<br />

7.4<br />

7.7<br />

6.9<br />

6.9<br />

9.0<br />

8.4<br />

8.5<br />

6.1<br />

8.1<br />

B.5<br />

8.2<br />

8.1<br />

7.4<br />

8.1<br />

7.0<br />

7.5<br />

7.3<br />

8.0<br />

7.2<br />

6.7<br />

8.1<br />

8.2<br />

8.1<br />

7.9<br />

8.7<br />

7.7<br />

TABLE<br />

CONC<br />

120.3<br />

140.2<br />

186.1<br />

125.1<br />

140.1<br />

149.7<br />

142.7<br />

159.5<br />

149.7<br />

114.4<br />

193.4<br />

76.6<br />

100.8<br />

76.7<br />

113.3<br />

135.7<br />

113.9<br />

91.2<br />

127.6<br />

126.9<br />

159.9<br />

133.0<br />

148.1<br />

136.6<br />

122.6<br />

212.3<br />

126.8<br />

120.0<br />

173.9<br />

207.5<br />

146.8<br />

151.3<br />

227.0<br />

124.9<br />

137.0<br />

128.2<br />

111.1<br />

126.2<br />

114.5<br />

156.8<br />

M.I.<br />

LIGHTS<br />

91.3<br />

95.8<br />

155.6<br />

94.8<br />

112.0<br />

116.1<br />

118.2<br />

111.0<br />

115.5<br />

81.4<br />

62.0<br />

53.5<br />

72.2<br />

56.3<br />

72.5<br />

113.5<br />

89.8<br />

62.2<br />

99.3<br />

99.8<br />

132.0<br />

105.0<br />

116.5<br />

108.2<br />

96.1<br />

188.3<br />

101.1<br />

96.3<br />

153.6<br />

182.3<br />

123.6<br />

129.5<br />

190.5<br />

101.1<br />

113.8<br />

99.1<br />

83.7<br />

94.6<br />

86.1<br />

129.5<br />

M.<br />

CONC.<br />

TOTAL<br />

29.0<br />

44.4<br />

30.5<br />

30.3<br />

28.1<br />

33.6<br />

24.5<br />

48.5<br />

34.2<br />

33.0<br />

131.4<br />

23.1<br />

28.6<br />

20.4<br />

40.8<br />

22.2<br />

24.1<br />

29.0<br />

28.3<br />

27.1<br />

27.9<br />

28.0<br />

31.6<br />

28.6<br />

26.5<br />

24.0<br />

25.7<br />

23.7<br />

20.3<br />

25.2<br />

23.2<br />

21.6<br />

36.5<br />

23.8<br />

23.2<br />

29.1<br />

27.4<br />

31.6<br />

28.4<br />

27.3<br />

I. CONC<br />

Essrsc — --<br />

NON<br />

MAG<br />

20.1<br />

28.8<br />

19.4<br />

20.1<br />

17.5<br />

20.7<br />

15.0<br />

33.8<br />

21.3<br />

21.3<br />

19.7<br />

12.6<br />

18.0<br />

12.6<br />

19.4<br />

12.7<br />

16.2<br />

17.8<br />

16.9<br />

16.5<br />

19.4<br />

17.1<br />

19.4<br />

17.5<br />

16.0<br />

14.8<br />

16.6<br />

14.5<br />

12.5<br />

15.6<br />

14.3<br />

13.1<br />

16.3<br />

16.3<br />

13.6<br />

18.0<br />

16.7<br />

19.8<br />

17.3<br />

16.9<br />

NO.<br />

MAG V.G.<br />

8.9<br />

15.6<br />

11.1<br />

10.2<br />

10.6<br />

12.9<br />

9.5<br />

14.7<br />

12.9<br />

11.7<br />

111.7<br />

10.5<br />

10.6<br />

7.8<br />

21.4<br />

9.5<br />

7.9<br />

11.2<br />

11.4<br />

10.6<br />

8.5<br />

10.9<br />

12.2<br />

11.1<br />

10.5<br />

9.2<br />

9.1<br />

9.2<br />

7.B<br />

9.6<br />

8.9<br />

8.7<br />

20.2<br />

7.5<br />

9.6<br />

11.1<br />

10.7<br />

11.6<br />

11.1<br />

10.4<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

6<br />

1<br />

4<br />

1<br />

0<br />

4<br />

0<br />

0 1 0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

1<br />

1<br />

0 1 0 1 0 1 3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0 1 CLAST MATRIX<br />

CALC i<br />

PPB<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

6691<br />

1850<br />

98<br />

161<br />

NA<br />

1659<br />

NA<br />

NA<br />

57<br />

NA<br />

NA<br />

NA<br />

88<br />

NA<br />

NA<br />

713<br />

3088<br />

NA<br />

26<br />

NA<br />

40()<br />

NA<br />

722<br />

5343<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

60<br />

SIZE<br />

l<br />

V/SGR<br />

TR<br />

TR<br />

P<br />

P<br />

P<br />

P<br />

P<br />

C<br />

C<br />

p r<br />

r, L<br />

C<br />

C<br />

P<br />

P<br />

P<br />

C<br />

P<br />

TR<br />

TR<br />

P<br />

C<br />

P<br />

C<br />

C<br />

C<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

NA<br />

NA<br />

70<br />

80<br />

60<br />

70<br />

80<br />

85<br />

70<br />

75<br />

85<br />

80<br />

80<br />

80<br />

40<br />

35<br />

25<br />

NA<br />

NA<br />

60<br />

60<br />

80"<br />

80<br />

85<br />

85<br />

80<br />

85<br />

90<br />

80<br />

80<br />

75<br />

70<br />

60<br />

70<br />

70<br />

70<br />

70<br />

70<br />

70<br />

70<br />

NA<br />

NA<br />

30<br />

20<br />

40<br />

30<br />

20<br />

15<br />

30<br />

25<br />

15<br />

20<br />

20<br />

20<br />

60<br />

60<br />

65<br />

NA<br />

NA<br />

40<br />

40<br />

20<br />

20<br />

15<br />

15<br />

20<br />

15<br />

10<br />

20<br />

20<br />

25<br />

30<br />

40<br />

30<br />

30<br />

30<br />

30<br />

30<br />

30<br />

30<br />

S/U<br />

LS<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

5<br />

10<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

TR<br />

TR<br />

TR<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

NA<br />

NA<br />

A<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

S<br />

S<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

S<br />

U<br />

U<br />

S<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

SD<br />

F<br />

F<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

M,F<br />

Y<br />

Y<br />

M,F<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

ST CY<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

N N<br />

Y N<br />

Y N<br />

Y N<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

Y Y<br />

Y<br />

Y<br />

COLOR<br />

SD<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

6B<br />

6B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

CY<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

6B<br />

GB<br />

B<br />

NA<br />

NA<br />

NA<br />

GB<br />

6B<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

B<br />

B B B<br />

B<br />

GB<br />

GB<br />

BN<br />

B<br />

B<br />

B<br />

B-<br />

B<br />

B<br />

SAND<br />

SAND<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

SAND<br />

TILL<br />

TILL<br />

SAND<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


1 1 ,<br />

^AGE 1<br />

COGEMA<br />

04<br />

1 11<br />

1<br />

1 111111111111<br />

cobo2apr.wri<br />

TOTAL it OF SAMPLES IN THIS REPORT s 40<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMF1E WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

M.<br />

CLAST<br />

TABLE<br />

SPLIT<br />

+10<br />

CHIPS<br />

TABLE<br />

FEED<br />

TABLE<br />

CONC<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

i. cote<br />

NON<br />

MAG<br />

— M*, i-<br />

NO.<br />

MAG V.G.<br />

CALC<br />

PPB<br />

MATRIX<br />

SIZE X S/U SD ST CY COLOR<br />

V/S GR LS OT SD CY<br />

CLASS<br />

60B-87<br />

24-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

25-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

26-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

26-12<br />

9.3<br />

8.3<br />

8.8<br />

9.6<br />

9.0<br />

9.0<br />

8.2<br />

9.0<br />

8.3<br />

9.4<br />

8.2<br />

8.2<br />

9.6<br />

9.4<br />

9.9<br />

8.9<br />

9.6<br />

9.6<br />

9.4<br />

9.4<br />

9.4<br />

6.8<br />

9.4<br />

7.0<br />

9.8<br />

9.1<br />

9.4<br />

5.0<br />

9.4<br />

9.5<br />

'9.5<br />

9.2<br />

9.3<br />

9.4<br />

9.6<br />

6.6<br />

9.7<br />

9.7<br />

9.0<br />

9.3<br />

1.2<br />

1.3<br />

0.9<br />

1.0<br />

0.6<br />

0.7<br />

0.9<br />

0.0<br />

0.0<br />

1.5<br />

1.3<br />

0.8<br />

1.0<br />

1.1<br />

1.5<br />

1.3<br />

1.2<br />

1.2<br />

0.3<br />

0.7<br />

0.5<br />

0.5<br />

1.1<br />

0.5<br />

0.7<br />

0.3<br />

1.3<br />

0.4<br />

1.3<br />

1.4<br />

1.2<br />

1.5<br />

0.7<br />

0.7<br />

1.0<br />

0.5<br />

0.9<br />

1.6<br />

1.2<br />

1.0<br />

8.1<br />

7.0<br />

7.9<br />

6.6<br />

8.4<br />

8.3<br />

7.3<br />

9.0<br />

8.3<br />

7.9<br />

6.9<br />

7.4<br />

8.6<br />

8.3<br />

8.4<br />

7.6<br />

6.4<br />

8.4<br />

9.1<br />

8.7<br />

8.9<br />

8.3<br />

8.3<br />

6.5<br />

9.1<br />

8.6<br />

8.1<br />

4.6<br />

B.I<br />

8.1<br />

8.3<br />

7.7<br />

6.6<br />

8.7<br />

8.6<br />

6.1<br />

8.6<br />

8.1<br />

7.8<br />

8.3<br />

113.8<br />

92.2<br />

132.7<br />

120.4<br />

123.2<br />

85.8<br />

84.6<br />

58.9<br />

117.1<br />

129.5<br />

119.9<br />

104.7<br />

11. l<br />

115.0<br />

111.9<br />

90.5<br />

76.9<br />

82.9<br />

80.4<br />

113.7<br />

128.1<br />

142.9<br />

107.5<br />

118.9<br />

118.0<br />

125.9<br />

130.9<br />

122.1<br />

150.1<br />

117.2<br />

175.7<br />

161.6<br />

173.6<br />

193.7<br />

188.3<br />

182.1<br />

157.5<br />

127.1<br />

127.4<br />

97.1<br />

90.1<br />

70.2<br />

110.1<br />

93.7<br />

96.1<br />

61.3<br />

68.4<br />

39.6<br />

97.7<br />

95.5<br />

100.0<br />

80.3<br />

53.9<br />

90.9<br />

86.6<br />

67.0<br />

55.9<br />

60.2<br />

63.0<br />

88.3<br />

96.6<br />

110.8<br />

79.1<br />

102.7<br />

92.4<br />

98.4<br />

95.6<br />

102.2<br />

121.0<br />

92.6<br />

147.5<br />

128.5<br />

146.2<br />

161.4<br />

151.5<br />

149.8<br />

124.4<br />

95.1<br />

98.2<br />

80.7<br />

23.7<br />

22.0<br />

22.6<br />

26.7<br />

27.1<br />

24.5<br />

16.2<br />

19.3<br />

19.4<br />

34.0<br />

19.9<br />

24.4<br />

23.3<br />

24.1<br />

25.3<br />

23.5<br />

23.0<br />

22.7<br />

17.4<br />

25.4<br />

31.5<br />

32.1<br />

28.4<br />

16.2<br />

25.6<br />

27.5<br />

35.3<br />

19.9<br />

29.1<br />

24.6<br />

26.2<br />

33.1<br />

27.4<br />

32.3<br />

36,8<br />

32.3<br />

33.1<br />

32.0<br />

29.2<br />

16.4<br />

33.9<br />

12.8<br />

13.6<br />

16.2<br />

16.1<br />

14.6<br />

10.0<br />

12.6<br />

11.9<br />

16.6<br />

10.9<br />

13.4<br />

14.3<br />

14.7<br />

15.4<br />

14.5<br />

13.3<br />

12.8<br />

11.0<br />

15.8<br />

19.5<br />

19.5<br />

15.5<br />

9.7<br />

15.9<br />

17.9<br />

19.3<br />

12.2<br />

17.0<br />

14.8<br />

16.7<br />

18.2<br />

16.3<br />

21.0<br />

25.3<br />

21.6<br />

22.2<br />

20.4<br />

19.3<br />

11.5<br />

9.6<br />

9.2<br />

6.8<br />

10.5<br />

11.0<br />

9.7<br />

6.2<br />

6.7<br />

7.5<br />

15.4<br />

9.0<br />

11.0<br />

9.0<br />

9.4<br />

9.9<br />

9.0<br />

9.7<br />

9.9<br />

6.4<br />

9.6<br />

12.0<br />

12.6<br />

12.9<br />

6.5<br />

9.7<br />

9.6<br />

16.0<br />

7.7<br />

12.1<br />

9.8<br />

11.5<br />

14.9<br />

11.1<br />

11.3<br />

11.5<br />

10.7<br />

10.9<br />

11.6<br />

9.9<br />

4.9<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

3<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

111<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

156<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

386<br />

323<br />

95<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

3313<br />

671<br />

334<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

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p<br />

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P<br />

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60<br />

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80<br />

75<br />

75<br />

60<br />

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70 4"0<br />

40<br />

70<br />

80<br />

60<br />

60<br />

80<br />

85<br />

85<br />

65<br />

85<br />

65<br />

80<br />

465<br />

85<br />

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80<br />

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80<br />

60<br />

80<br />

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70<br />

75<br />

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64<br />

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75 TR<br />

20 TR<br />

25 NA<br />

25 TR<br />

20 TR<br />

20 TR<br />

NA NA<br />

NA NA<br />

30 NA<br />

60 NA<br />

60 NA<br />

30 NA<br />

20 NA<br />

10 10<br />

10 10<br />

16<br />

14<br />

14<br />

14<br />

14<br />

15 TR<br />

20 TR<br />

35 TR<br />

15 TR<br />

20 TR<br />

20 TR<br />

20 TR<br />

15 15<br />

15 5<br />

19 1<br />

19<br />

19 1<br />

20 5<br />

10 15<br />

15 5<br />

15 5<br />

35 1<br />

34 1<br />

25 40<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

S Y<br />

S Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

Y Y GB 6B<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y GB B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y GB B<br />

Y Y B B<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y GB GB<br />

Y "Y<br />

GB GB<br />

Y Y GB GB<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y GB GY<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

Y Y B B<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

SAND<br />

SANDULD<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


l<br />

PAGE 1 CQGEMA 04;<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

COB03APR.WRI<br />

TOTAL i OF SAMPLES IN THIS REPORT = 40<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

BOB-87<br />

26-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

-21<br />

-22<br />

-23<br />

27-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

28-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

29-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

29-08<br />

TABLE<br />

Cpl IT<br />

or L 1 1<br />

9.8<br />

9.7<br />

9.8<br />

10.0<br />

10.1<br />

9.9<br />

9.6<br />

9.1<br />

6.6<br />

9.3<br />

9.1<br />

7.7<br />

9.6<br />

7.3<br />

9.7<br />

9.7<br />

9.0<br />

9.0<br />

9.3<br />

9.5<br />

8.5<br />

8.2<br />

9.3<br />

9.0<br />

8.7<br />

8.7<br />

7.2<br />

9.4<br />

7.3<br />

8.4<br />

8.4<br />

B. 3<br />

9.1<br />

9.8<br />

9.4<br />

9.4<br />

9.7<br />

9.3<br />

9.7<br />

9.7<br />

+10<br />

PU T PC<br />

Lniro<br />

1.0<br />

2.4<br />

1.6<br />

1.9<br />

2.0<br />

1.9<br />

2.0<br />

1.6<br />

0.5<br />

1.1<br />

1.4<br />

1.4<br />

1.0<br />

0.4<br />

1.7<br />

2.2<br />

0.8<br />

1.4<br />

1.3<br />

1.5<br />

0.8<br />

0.6<br />

0.4<br />

0.3<br />

0.4<br />

1.0<br />

0.6<br />

0.9<br />

0.5<br />

0.4<br />

0.6<br />

0.6<br />

0.8<br />

1.2<br />

1.6<br />

1.1<br />

1.6<br />

0.8<br />

0.8<br />

1.4<br />

TABLE<br />

FEED<br />

8.8<br />

7.3<br />

8.2<br />

6.1<br />

8.1<br />

8.0<br />

7.6<br />

7.5<br />

6.1<br />

8.2<br />

7.7<br />

6.3<br />

8.6<br />

6.9<br />

8.0<br />

7.5<br />

8.2<br />

7.6<br />

8.0<br />

8.0<br />

7.7<br />

7.6<br />

8.9<br />

8.7<br />

6.3<br />

7.7<br />

6.6<br />

8.5<br />

6.8<br />

8.0<br />

7.8<br />

7.7<br />

8.3<br />

8.6<br />

7.8<br />

8.3<br />

8.1<br />

8.5<br />

8.9<br />

8.3<br />

TABLE<br />

CONC<br />

68.0<br />

150.1<br />

197.4<br />

134.9<br />

96.6<br />

179.3<br />

179.1<br />

254.8<br />

137.3<br />

199.4<br />

156.6<br />

150.5<br />

156.3<br />

137.2<br />

165.7<br />

170.3<br />

196.6<br />

121.9<br />

168.2<br />

121.3<br />

125.4<br />

85.7<br />

74.7<br />

113.0<br />

131.5<br />

170.1<br />

161.4<br />

254.4<br />

191.8<br />

190.2<br />

197.9<br />

201.5<br />

193.6<br />

201.6<br />

213.0<br />

220.1<br />

205.4<br />

239.5<br />

106.3<br />

123.3<br />

M.I.<br />

CONC.<br />

1 TEUTC TnTAi<br />

L ion 13 IUIHL<br />

73.4<br />

123.5<br />

170.5<br />

115.1<br />

70.7<br />

136.5<br />

147.9<br />

228.5<br />

115.8<br />

175.8<br />

126.1<br />

101.9<br />

127.4<br />

112.6<br />

129.2<br />

137.5<br />

160.6<br />

94.7<br />

134.7<br />

92.5<br />

99.4<br />

62.5<br />

51.6<br />

87.2<br />

107.4<br />

144.9<br />

141.6<br />

228.6<br />

173.9<br />

174.3<br />

178.2<br />

179.9<br />

162.4<br />

165.5<br />

182.7<br />

185.7<br />

170.7<br />

202.7<br />

70.4<br />

94.6<br />

M. I. CONC CLAST MATRIX<br />

14.6<br />

26.6<br />

26.9<br />

19.8<br />

25,9<br />

42.8<br />

31.2<br />

26.3<br />

21.5<br />

23.6<br />

30.5<br />

48.6<br />

28.9<br />

24.6<br />

36.5<br />

32.8<br />

36.2<br />

27.2<br />

33.5<br />

28.8<br />

26.0<br />

23.2<br />

23.1<br />

25.8<br />

24.1<br />

25.2<br />

19.8<br />

25.B<br />

17.9<br />

15.9<br />

19.7<br />

21.6<br />

31.4<br />

36.1<br />

30.3<br />

34.4<br />

34.7<br />

36.8<br />

35.9<br />

28.7<br />

NON<br />

ij An<br />

MAG<br />

10.6<br />

16.3<br />

16.6<br />

12.8<br />

15.4<br />

21.9<br />

16.6<br />

18.5<br />

14.3<br />

15.4<br />

16.8<br />

29.6<br />

19.3<br />

16.6<br />

22.4<br />

20.5<br />

22.7<br />

16.0<br />

20.7<br />

17.0<br />

15.9<br />

14.4<br />

14.9<br />

15.3<br />

15.0<br />

17.0<br />

13.9<br />

17.0<br />

11.5<br />

11.1<br />

13.8<br />

16.1<br />

19.4<br />

24.5<br />

20.4<br />

22.3<br />

21.9<br />

25.2<br />

25.5<br />

17.5<br />

NO.<br />

U/tn li ft<br />

MAS V.G.<br />

4.0<br />

10.3<br />

10.3<br />

7.0<br />

10.5<br />

20.9<br />

12.4<br />

7.6<br />

7.2<br />

6.2<br />

11.7<br />

19.0<br />

9.6<br />

8.0<br />

14.1<br />

12.3<br />

13.5<br />

11.2<br />

12.8<br />

11.6<br />

KM<br />

6.6<br />

8.2<br />

10.5<br />

9.1<br />

6.2<br />

5.9<br />

6.8<br />

6.4<br />

4.6<br />

5.9<br />

5.5<br />

12.0<br />

11.6<br />

9.9<br />

12.1<br />

12.8<br />

11.6<br />

10.4<br />

11.2<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

5<br />

3<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

2<br />

0<br />

0<br />

CALC SIZE X S/U SD ST CY COLOR<br />

rrtf —————<br />

V/SGR LS OT<br />

SD CY<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

731 P<br />

NA P<br />

115 P<br />

NA C<br />

NA P<br />

m P<br />

NA C<br />

NA P<br />

NA P, C<br />

NA P<br />

1265 P<br />

527 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

201 P<br />

NA P<br />

NA P<br />

67 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

4579 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA C<br />

NA C<br />

NA P<br />

124 P<br />

NA P<br />

NA P<br />

65 5<br />

55 30<br />

60 30<br />

70 25<br />

74 25<br />

85 14<br />

85 15<br />

80 20<br />

90 10<br />

70 30<br />

60 40<br />

80 20<br />

70 30<br />

25 75<br />

55 40<br />

45 50<br />

60 40<br />

50 50<br />

70 30<br />

60 40<br />

60 40<br />

60 40<br />

40 60<br />

40 60<br />

60 40<br />

40 60<br />

65 35<br />

70 30<br />

40 60<br />

60 40<br />

60 40<br />

90 10<br />

60 40<br />

60 40<br />

60 35<br />

35 60<br />

40 60<br />

60 40<br />

30 70<br />

40 60<br />

30 NA<br />

15 NA<br />

10 NA<br />

5 NA<br />

1 NA<br />

1 NA<br />

TR NA<br />

NA NA<br />

NA NA<br />

TR NA<br />

TR NA<br />

NA NA<br />

TR NA<br />

NA NA<br />

5 NA<br />

5 NA<br />

TR NA<br />

NA NA<br />

TR NA<br />

TR NA<br />

TR NA<br />

TR A<br />

TR A<br />

TR A<br />

TR A<br />

NA A<br />

TR A<br />

TR A<br />

TR A<br />

NA NA<br />

NA A<br />

NA A<br />

TR NA<br />

TR NA<br />

5 NA<br />

5 NA<br />

TR NA<br />

Tfi NA<br />

TR NA<br />

TR NA<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

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U U<br />

U U<br />

U U<br />

U U<br />

U U<br />

U U GB GB TILL<br />

U N GB N TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U GB GB TILL<br />

U U B B TILL<br />

U U B B TILL<br />

U U B B TILL<br />

U U B B TILL<br />

U U GB B TILL<br />

U U B B TILL<br />

U U B B TILL<br />

U U B B TILL<br />

U U B B TILL<br />

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U U B GB TILL<br />

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l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

ME i COGEMA 04/<br />

COB04APR.WRI<br />

OVERBURDEN DRILLING HANAGEMENT LIMITED<br />

TOTAL f OF SAMPLES IN THIS REPORT = 40<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG.WET) WEIGHT (GRAMS DRV) AU DESCRIPTION CLASS<br />

NU. :<br />

BOB-87<br />

29-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

30-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

31-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

31-13<br />

TABLE<br />

SPLIT<br />

9.3<br />

8.8<br />

9.4<br />

9.4<br />

8.6<br />

9.5<br />

9.0<br />

6.2<br />

7.9<br />

9.5<br />

9.5<br />

8.0<br />

9.1<br />

6.1<br />

6.6<br />

9.1<br />

9.0<br />

9.0<br />

8.6<br />

9.8<br />

6.4<br />

9.3<br />

9.2<br />

9.0<br />

9.3<br />

8.4<br />

8.7<br />

4.7<br />

7.4<br />

8.8<br />

9.4<br />

9.5<br />

9.2<br />

9.9<br />

9.8<br />

8.4<br />

9.1<br />

8.7<br />

9.1<br />

9.1<br />

+10<br />

CHIPS<br />

1.2<br />

0.6<br />

1.2<br />

1.1<br />

0.5<br />

0.9<br />

1.0<br />

1.5<br />

1.0<br />

1.4<br />

1.4<br />

0.4<br />

2.0<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.7<br />

1.0<br />

0.4<br />

0.0<br />

0.6<br />

0.2<br />

0.2<br />

0.3<br />

0.1<br />

0.4<br />

0.4<br />

0.3<br />

1.2<br />

1.0<br />

0.4<br />

0.8<br />

0.5<br />

0.4<br />

0.7<br />

0.4<br />

0.5<br />

1.2<br />

TABLE<br />

FEED<br />

8.1<br />

8.2<br />

8.2<br />

8.3<br />

8.1<br />

6.6<br />

8.0<br />

4.7<br />

6.9<br />

8.1<br />

8.1<br />

7.6<br />

7.1<br />

5.7<br />

6.2<br />

8.7<br />

8.6<br />

6.6<br />

7.9<br />

8.8<br />

6.0<br />

9.3<br />

8.6<br />

8.6<br />

9.1<br />

e.i<br />

8.6<br />

4.3<br />

7.0<br />

8,5<br />

8.2<br />

8.5<br />

8.8<br />

9.1<br />

9.3<br />

8.0<br />

8.4<br />

8.3<br />

8.6<br />

7.9<br />

TABLE<br />

CONC<br />

138.1<br />

98.5<br />

202.2<br />

94.3<br />

75.5<br />

133.0<br />

287.6<br />

106.3<br />

87.7<br />

160.6<br />

74.8<br />

94.1<br />

129.8<br />

94.7<br />

148.7<br />

214.6<br />

187.8<br />

164.4<br />

188.5<br />

178.7<br />

145.6<br />

175.2<br />

286.5<br />

302.7<br />

243.2<br />

116.9<br />

112.3<br />

61.4<br />

61.9<br />

146.0<br />

139.5<br />

118.3<br />

82.3<br />

126.1<br />

94.1<br />

94.0<br />

124.5<br />

106.0<br />

92.4<br />

166.8<br />

M,<br />

M.I.<br />

CONC.<br />

LIGHTS TOTAL<br />

115.3<br />

68.1<br />

171.4<br />

63.0<br />

51.5<br />

108.2<br />

257.8<br />

79.7<br />

62.8<br />

127.0<br />

53.3<br />

69.5<br />

106.7<br />

67.8<br />

130.7<br />

188.3<br />

163.7<br />

134.7<br />

168.3<br />

153.2<br />

132.9<br />

140.9<br />

272.2<br />

287.4<br />

214.3<br />

85.0<br />

85.6<br />

46.5<br />

40.7<br />

120.8<br />

111.6<br />

90.7<br />

58.2<br />

95.2<br />

72.6<br />

68.3<br />

96.3<br />

81.1<br />

64.4<br />

135.6<br />

22.8<br />

30.4<br />

30.8<br />

31.3<br />

24.0<br />

24.6<br />

29. B<br />

26.6<br />

24.9<br />

33.6<br />

21.5<br />

24.6<br />

23.1<br />

26.9<br />

18.0<br />

26.3<br />

24.1<br />

29.7<br />

20.2<br />

25.5<br />

12.7<br />

34.3<br />

14.3<br />

15.3<br />

28.9<br />

31.9<br />

26.7<br />

14.9<br />

21.2<br />

25.2<br />

27.7<br />

27.6<br />

24.1<br />

30.9<br />

21.5<br />

25.7<br />

28.2<br />

24.9<br />

28.0<br />

31.2<br />

I. CONC<br />

NON<br />

MAG<br />

14.3<br />

20.0<br />

17.3<br />

16.9<br />

14.9<br />

15.6<br />

16.6<br />

15.4<br />

16.2<br />

22.5<br />

13.4<br />

14.9<br />

13.5<br />

19.5<br />

11.5<br />

16.5<br />

14.4<br />

17.0<br />

11.5<br />

14.9<br />

7.5<br />

20.6<br />

9.3<br />

10.2<br />

17.3<br />

20.1<br />

16.4<br />

9.7<br />

13.3<br />

17.0<br />

18.6<br />

18.4<br />

15.2<br />

18.4<br />

14.4<br />

16.8<br />

16.6<br />

16.1<br />

17.3<br />

20.6<br />

NO.<br />

MAG V.G.<br />

8.5<br />

10.4<br />

13.5<br />

14.4<br />

9.1<br />

9.2<br />

13.2<br />

11.2<br />

8.7<br />

11.1<br />

8.1<br />

9.7<br />

9.6<br />

7.4<br />

6.5<br />

9.6<br />

9.7<br />

12.7<br />

6.7<br />

10.6<br />

5.2<br />

13.7<br />

5.0<br />

5,1<br />

11.6<br />

11.8<br />

10.3<br />

5.2<br />

7.9<br />

8.2<br />

8.9<br />

9.2<br />

8.9<br />

12.5<br />

7.1<br />

8.9<br />

11.6<br />

8.8<br />

10.7<br />

10.6<br />

0<br />

0<br />

0<br />

0<br />

1<br />

1<br />

0<br />

1<br />

0<br />

5<br />

5<br />

.1<br />

0<br />

0<br />

0<br />

0 1 0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0 1 0<br />

0<br />

0<br />

CALC<br />

PPB<br />

NA<br />

NA<br />

NA<br />

NA<br />

25<br />

3607<br />

NA<br />

11099<br />

NA<br />

326<br />

215<br />

519<br />

NA<br />

NA<br />

NA<br />

NA<br />

1506<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

4110<br />

NA<br />

NA<br />

NA<br />

1<br />

SIZE<br />

\<br />

P<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P,BL<br />

p<br />

P<br />

C<br />

P,C<br />

p p p TR<br />

P,C<br />

C<br />

P<br />

P<br />

P,6K<br />

P<br />

p r<br />

p .<br />

p<br />

p p<br />

P,C<br />

p c c p<br />

p<br />

p<br />

1AST<br />

y.<br />

//S GR<br />

30<br />

40<br />

40<br />

45<br />

M<br />

65<br />

45<br />

44<br />

50<br />

45<br />

35<br />

50<br />

60<br />

95<br />

39<br />

45<br />

60<br />

80<br />

70<br />

55<br />

55<br />

NA<br />

50<br />

10<br />

20<br />

55<br />

95<br />

45<br />

"55]<br />

60;<br />

60<br />

60<br />

65<br />

65<br />

60<br />

60<br />

60<br />

60<br />

50<br />

35;<br />

70<br />

60<br />

60<br />

55<br />

70<br />

35<br />

55<br />

55<br />

50<br />

55<br />

65<br />

50<br />

39<br />

4<br />

60<br />

50<br />

40<br />

20<br />

30<br />

45<br />

45<br />

NA<br />

50<br />

90<br />

80<br />

45<br />

5<br />

55<br />

40<br />

40<br />

40<br />

40<br />

35<br />

35<br />

40<br />

40<br />

40<br />

40<br />

50<br />

65<br />

:sss<br />

sszr<br />

LS<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

NA<br />

TR<br />

1<br />

TR<br />

TR<br />

NA<br />

TR<br />

1<br />

1<br />

1<br />

5<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

5<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

MAT!<br />

sssssss<br />

S/USD<br />

u<br />

y uuuuuuuuuuuuuuuuuuusuuuuuuuuuuuuuuuuuu<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

F<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

RIX<br />

ST<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y'<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

CY COLOR<br />

SD CY<br />

Y GB<br />

Y<br />

GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y<br />

B<br />

Y B<br />

Y<br />

B<br />

Y B<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y 6<br />

Y B<br />

Y B<br />

Y B<br />

'Y B<br />

Y B<br />

Y GB<br />

Y GB<br />

Y<br />

B<br />

Y B<br />

Y<br />

GB<br />

Y 6Y<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y<br />

B<br />

Y GB<br />

Y GB<br />

Y<br />

GB<br />

Y GB<br />

Y<br />

GB<br />

Y<br />

B<br />

Y<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

66<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

B<br />

B<br />

GB<br />

GY<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

SAND<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE i<br />

COB05APR.WRI<br />

TOTAL K OF SAMPLES IN THIS REPORT = 40<br />

SAMPLE<br />

WEIGHT (KG.WET)<br />

C06EMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

NU.<br />

BOB-87<br />

31-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

-21<br />

-22<br />

-23<br />

32-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

33-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

34-01<br />

-02<br />

34-03<br />

TABLE<br />

SPLIT<br />

9.2<br />

9.4<br />

9.1<br />

8.8<br />

9.4<br />

9.7<br />

9.5<br />

9.0<br />

9.0<br />

8.7<br />

8.9<br />

9.7<br />

9.8<br />

9.3<br />

7.2<br />

9.7<br />

9.5<br />

7.6<br />

9.4<br />

7.5<br />

10.1<br />

9.2<br />

8.3<br />

8.8<br />

8.8<br />

9.5<br />

10.0<br />

10.1<br />

9.2<br />

8.1<br />

9.1<br />

9.9<br />

9.8<br />

9.8<br />

9.5<br />

9.7<br />

9.5<br />

9.5<br />

4.9<br />

8.6<br />

+IO<br />

PU T DC<br />

LnlrS<br />

0.4<br />

0.6<br />

1.2<br />

0.8<br />

0.9<br />

2.2<br />

0.8<br />

0.5<br />

0.6<br />

0.5<br />

2.1<br />

1.2<br />

1.0<br />

1.0<br />

0.6<br />

0.5<br />

0.6<br />

0.5<br />

0.6<br />

0.2<br />

1.3<br />

0.8<br />

0.6<br />

0.1<br />

0.0<br />

2.2<br />

3.1<br />

3.5<br />

1.6<br />

0.4<br />

1.3<br />

2.0<br />

1.2<br />

0.9<br />

0.9<br />

0.2<br />

0.5<br />

0.9<br />

0.3<br />

0.6<br />

TABLE<br />

FEED<br />

8.8<br />

e. 6<br />

7.9<br />

8.0<br />

8.5<br />

7.5<br />

8.7<br />

8.5<br />

8.4<br />

8.2<br />

6.6<br />

8.5<br />

8.8<br />

8.3<br />

6.6<br />

9.2<br />

8.9<br />

7.1<br />

8.8<br />

7.3<br />

8.6<br />

8.4<br />

7.7<br />

8.7<br />

8.6<br />

7.3<br />

6.9<br />

6.6<br />

7.6<br />

7.7<br />

7.6<br />

7.9<br />

B. 6<br />

8.9<br />

8.6<br />

9.5<br />

9.0<br />

8.6<br />

4.6<br />

8.0<br />

TABLE<br />

cone<br />

137.5<br />

134.8<br />

199.1<br />

182.6<br />

129.6<br />

176.3<br />

225.5<br />

98.0<br />

174.4<br />

198.4<br />

221.2<br />

177.9<br />

160.6<br />

177.0<br />

130.8<br />

146.8<br />

110.4<br />

77.9<br />

107.0<br />

74.6<br />

124.7<br />

109.2<br />

122.1<br />

162.1<br />

99.7<br />

95.3<br />

294.1<br />

266.1<br />

200.3<br />

82.8<br />

96.1<br />

174.2<br />

76.2<br />

96.0<br />

72.9<br />

76.2<br />

60.5<br />

76.5<br />

71.8<br />

75.1<br />

M.I.<br />

LIGHTS<br />

109.9<br />

109.5<br />

174.2<br />

155.5<br />

102.3<br />

141.1<br />

202.9<br />

70.8<br />

136.9<br />

167.1<br />

186.8<br />

151.3<br />

152.3<br />

153.5<br />

110.9<br />

119.6<br />

83.7<br />

58.7<br />

63.4<br />

60.5<br />

97.0<br />

85.7<br />

97.1<br />

147.6<br />

87.2<br />

68.9<br />

257.9<br />

231.4<br />

172.5<br />

58.2<br />

70.6<br />

157.4<br />

59.3<br />

69.5<br />

52.0<br />

63.3<br />

43.7<br />

54.4<br />

59.8<br />

50.9<br />

M.<br />

CONC.<br />

TOTAL<br />

27.6<br />

25.3<br />

24.9<br />

27.1<br />

27.3<br />

37.2<br />

22.6<br />

27.2<br />

35.5<br />

31.3<br />

34.4<br />

26.6<br />

28.3<br />

23.5<br />

19.9<br />

27.2<br />

26.7<br />

19.2<br />

"23.6<br />

14.3<br />

27.7<br />

23.5<br />

25.0<br />

14.5<br />

12.5<br />

26.4<br />

36.2<br />

34.7<br />

27.8<br />

24.6<br />

25.5<br />

16.8<br />

16.9<br />

26.5<br />

20.9<br />

12.9<br />

16.8<br />

22.1<br />

12.0<br />

24.2<br />

I. CON<br />

NON<br />

MAP<br />

HAG<br />

17.8<br />

15.9<br />

15.6<br />

18.6<br />

17.9<br />

23.7<br />

15.0<br />

19.1<br />

25.8<br />

22.5<br />

22.1<br />

16.6<br />

16.1<br />

15.4<br />

12.8<br />

17.4<br />

16.5<br />

12.7<br />

15.5<br />

10.3<br />

17.4<br />

14.9<br />

15.6<br />

9.2<br />

7.9<br />

14.4<br />

21.6<br />

21.1<br />

17,6<br />

15.2<br />

16.1<br />

11.0<br />

10.2<br />

16.5<br />

12.7<br />

5.2<br />

10.8<br />

13.2<br />

7.9<br />

14.2<br />

C<br />

l<br />

MAC 1<br />

nnU<br />

i<br />

9.8<br />

9.4<br />

9.3<br />

8.5<br />

9.4<br />

13.5<br />

7.6<br />

8.1<br />

9.7<br />

8.6<br />

12.3<br />

10.0<br />

10.2<br />

8.1<br />

7.1<br />

9.8<br />

10,2<br />

6.5<br />

8.1<br />

4.0<br />

10.3<br />

8.6<br />

9.2<br />

5.3<br />

4.6<br />

12.0<br />

14.6<br />

13.6<br />

10.0<br />

9.4<br />

9.4<br />

5.8<br />

6.7<br />

10.0<br />

8.2<br />

7.7<br />

6.0<br />

8.9<br />

4.1<br />

10.0<br />

ffi.<br />

.6.<br />

1<br />

4<br />

1<br />

0<br />

3<br />

0<br />

0<br />

0 0 0<br />

1<br />

0<br />

0<br />

0 01 0<br />

0<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

5 1 0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

CALC<br />

PPR<br />

rrp<br />

277<br />

824<br />

731<br />

NA<br />

1430<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

1268<br />

NA<br />

NA<br />

NA<br />

NA<br />

358<br />

NA<br />

NA<br />

517<br />

NA m NA<br />

NA<br />

NA<br />

NA<br />

104<br />

14930<br />

161<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

ST*"""<br />

SIZ<br />

p<br />

c<br />

p<br />

6<br />

TR<br />

P<br />

P<br />

P P P<br />

P<br />

c<br />

P<br />

C P P<br />

P<br />

P<br />

C,B<br />

P<br />

P<br />

P<br />

P<br />

6<br />

TR<br />

P<br />

P<br />

P p p<br />

P<br />

C<br />

P<br />

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P<br />

P<br />

P'<br />

C,E<br />

P<br />

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CLAS1<br />

E<br />

V/SI<br />

45!<br />

i 60 !<br />

60'<br />

i 60!<br />

leo1<br />

|M<br />

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,60<br />

i 70,<br />

JTOi<br />

•15]<br />

35;<br />

30;<br />

35;<br />

35,<br />

40j<br />

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^45 i<br />

L50J<br />

50-.<br />

B5J<br />

90;<br />

90i<br />

"ffi<br />

fjM<br />

^i<br />

75<br />

70<br />

80<br />

60<br />

70<br />

75<br />

75<br />

85<br />

70<br />

35<br />

35<br />

'35<br />

L 20<br />

45<br />

r<br />

y.<br />

3R<br />

55<br />

40<br />

40<br />

40<br />

20<br />

20<br />

30<br />

35<br />

30<br />

30<br />

40<br />

60<br />

65<br />

65<br />

65<br />

60<br />

70<br />

55<br />

50<br />

50<br />

14<br />

10<br />

10<br />

90<br />

NA<br />

15<br />

14<br />

30<br />

20<br />

30<br />

30<br />

24<br />

24<br />

15<br />

30<br />

65<br />

65<br />

65<br />

80<br />

55<br />

sscc<br />

LS<br />

TR<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA 5<br />

TR<br />

TR<br />

5<br />

5<br />

5<br />

NA<br />

TR<br />

NA<br />

NA<br />

NA<br />

TR<br />

TR<br />

1<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

1<br />

TR<br />

NA<br />

10<br />

TR<br />

1<br />

1<br />

NA<br />

NA<br />

TR<br />

TR<br />

NA<br />

NA<br />

NA<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

A<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

S/U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

MAT<br />

SD<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

RIK<br />

ST<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

CY<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

N<br />

N<br />

N<br />

N<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

COL<br />

SD<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

OR<br />

CY<br />

B<br />

TILL<br />

GB TILL<br />

B<br />

TILL<br />

B<br />

TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B<br />

TILL<br />

B<br />

TILL<br />

B<br />

TILL<br />

B<br />

TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B<br />

J4tt SA'ii.<br />

GB tttr^.Nl<br />

N<br />

TILL<br />

N<br />

TILL<br />

N<br />

TILL<br />

N<br />

TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B<br />

TILL<br />

B<br />

TILL<br />

B<br />

TILL


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

IAGE i<br />

COB06APft.WRI<br />

TOTAL l OF SAMPLES IN THIS REPORT = 40<br />

COGEfIA<br />

OVERBURDEN DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

04/<br />

N'J.<br />

BGB-87<br />

34-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

35-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

36-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-H<br />

-12<br />

-13<br />

-14<br />

-15<br />

37-01<br />

37-02<br />

'ABLE<br />

SPLIT<br />

9.4<br />

8.0<br />

9.0<br />

9.4<br />

9.8<br />

9.4<br />

9.7<br />

9.7<br />

10.0<br />

9.1<br />

9.6<br />

10.2<br />

9.9<br />

9.9<br />

10.1<br />

9.7<br />

10.0<br />

9.8<br />

10.5<br />

10.0<br />

9.5<br />

10.2<br />

10.0<br />

9.5<br />

10.0<br />

10.2<br />

10.6<br />

10.2<br />

9.9<br />

10.0<br />

9.8<br />

10.1<br />

10.1<br />

10.2<br />

9.8<br />

9.2<br />

9.8<br />

10. 1<br />

9.5<br />

10.0<br />

+10<br />

CHIPS<br />

0.4<br />

0.4<br />

0.6<br />

0.5<br />

0.8<br />

0.4<br />

0.0<br />

0.4<br />

0.9<br />

1.0<br />

0.4<br />

0.8<br />

0.4<br />

0.5<br />

0.6<br />

0.8<br />

1.7<br />

1.8<br />

1.7<br />

1.5<br />

0.8<br />

0.6<br />

1.2<br />

1.4<br />

1.6<br />

1.8<br />

1.0<br />

1.4<br />

1.4<br />

1.7<br />

1.4<br />

0.7<br />

0.4<br />

0.2<br />

0.1<br />

0.1<br />

0.1<br />

0.6<br />

1.4<br />

1.2<br />

TABLE<br />

FEED<br />

9.0<br />

7.6<br />

6.4<br />

8.9<br />

9.0<br />

9.0<br />

9.7<br />

9.3<br />

9.1<br />

8.1<br />

9.2<br />

9.4<br />

9.5<br />

9.4<br />

9.5<br />

8.9<br />

8.3<br />

8.0<br />

8.8<br />

8.5<br />

8.7<br />

9.6<br />

8.8<br />

8.1<br />

8.4<br />

8.4<br />

9.6<br />

8.8<br />

8.5<br />

8.3<br />

8.4<br />

9.4<br />

9.7<br />

10.0<br />

9.7<br />

9.1<br />

9.7<br />

9.5<br />

8,1<br />

8.8<br />

TABLE<br />

CONC<br />

61.1<br />

65.8<br />

76.1<br />

12S.5<br />

92.6<br />

74.4<br />

77.7<br />

128.5<br />

166.7<br />

187.6<br />

88.0<br />

130.3<br />

103.0<br />

119.2<br />

76.9<br />

109.2<br />

132.3<br />

120.4<br />

76.2<br />

121.0<br />

100.3<br />

96.4<br />

102.4<br />

94.3<br />

131.0<br />

83.2<br />

105.9<br />

130.9<br />

88.9<br />

138.0<br />

190.2<br />

238.4<br />

258.2<br />

124.1<br />

179.6<br />

151.8<br />

175.9<br />

209.2<br />

241.5<br />

149.2<br />

H. I. CONC<br />

M.I. CONC. tiOH NO.<br />

LIGHTS TOTAL MAG MAG V.G.<br />

40.4<br />

47.0<br />

57.2<br />

91.8<br />

71.5<br />

55.7<br />

59.2<br />

303.7<br />

123.3<br />

157.6<br />

61.1<br />

106.3<br />

77.0<br />

89.0<br />

55.4<br />

98.3<br />

81.2<br />

84.6<br />

53.0<br />

99.5<br />

83.6<br />

70.9<br />

69.6<br />

70.8<br />

101.6<br />

54.5<br />

80.5<br />

99.8<br />

65.7<br />

120.9<br />

168.3<br />

219.5<br />

242.5<br />

107.8<br />

155.4<br />

135.1<br />

151.7<br />

177.7<br />

211.5<br />

141.8<br />

20.7<br />

18.8<br />

18.9<br />

29.7<br />

21.1<br />

18.7<br />

18.5<br />

24.8<br />

43.4<br />

30.0<br />

26.9<br />

24.0<br />

26.0<br />

30.2<br />

21.5<br />

10.9<br />

51.1<br />

35.6<br />

23.2<br />

21.5<br />

16.7<br />

25.5<br />

32.6<br />

23.5<br />

29.2<br />

33.7<br />

25.4<br />

31.1<br />

23.2<br />

17.1<br />

21.9<br />

18.9<br />

15.7<br />

16.3<br />

24.2<br />

16.7<br />

24.2<br />

31.5<br />

30.0<br />

27.4<br />

13.1<br />

12.6<br />

12.2<br />

15.9<br />

12.1<br />

11.4<br />

12.3<br />

16.2<br />

30.4<br />

22,2<br />

17.6<br />

14.4<br />

15.4<br />

17.0<br />

13.3<br />

7.4<br />

26.9<br />

18.9<br />

13,5<br />

13.0<br />

6.2<br />

34.6<br />

19.0<br />

12.9<br />

16.3<br />

19.9<br />

14.5<br />

16.0<br />

13,2<br />

9.9<br />

15,1<br />

13.4<br />

13.3<br />

12.2<br />

17.0<br />

13.3<br />

17.0<br />

20.3<br />

19.2<br />

17.8<br />

7.6<br />

6.2<br />

6.7<br />

13.8<br />

9.0<br />

7.3<br />

6.2<br />

8,6<br />

13.0<br />

7.6<br />

9.3<br />

9.6<br />

10.6<br />

13.2<br />

8.2<br />

3.5<br />

24.2<br />

16.7<br />

9.7<br />

8.5<br />

10.5<br />

10.9<br />

13.8<br />

10.6<br />

12.9<br />

13.6<br />

10.9<br />

15.1<br />

10.0<br />

7.2<br />

6.8<br />

5.5<br />

2.4<br />

4.1<br />

7.2<br />

3.4<br />

7.2<br />

11.2<br />

10.8<br />

9.6<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0 1 0<br />

0<br />

0<br />

0 1 0 1 3<br />

6<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

4<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0 11 0<br />

0 1 0<br />

:rss:z srzszsszrrsssssr<br />

CLAST<br />

CALC<br />

PPB<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

281<br />

KA<br />

NA<br />

NA<br />

NA<br />

371<br />

NA<br />

79<br />

766<br />

1242<br />

NA<br />

163<br />

145<br />

NA<br />

NA<br />

NA<br />

NA<br />

296<br />

308<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

38<br />

76<br />

NA<br />

NA<br />

151<br />

NA<br />

SIZE<br />

l<br />

V/S GR<br />

C '<br />

c -<br />

C .<br />

P p p<br />

TR<br />

P<br />

C<br />

P<br />

P<br />

P<br />

P<br />

15<br />

70<br />

sp;<br />

45 1<br />

56,<br />

45<br />

ta;<br />

Kfc<br />

95 j<br />

80!<br />

50 i<br />

45<br />

55|<br />

p<br />

m<br />

c<br />

p<br />

p<br />

F<br />

P<br />

p<br />

P/C<br />

P<br />

P<br />

C<br />

P, H.<br />

P,C<br />

P,C<br />

P,C<br />

c c<br />

P,C<br />

P, C<br />

P,C<br />

p p p<br />

F<br />

P<br />

P<br />

p<br />

50<br />

45<br />

50<br />

60<br />

60<br />

60<br />

80<br />

70<br />

50<br />

85<br />

85<br />

90<br />

85<br />

85<br />

80<br />

70<br />

70<br />

90<br />

90<br />

75<br />

85<br />

85<br />

85<br />

70<br />

40<br />

35<br />

85<br />

30<br />

50<br />

55<br />

50<br />

55<br />

NA<br />

20<br />

5<br />

20<br />

50<br />

55<br />

45<br />

50<br />

50<br />

55<br />

50<br />

39<br />

40<br />

40<br />

2-0<br />

30<br />

5*)<br />

15<br />

15<br />

10<br />

15<br />

15<br />

20<br />

30<br />

30<br />

10<br />

10<br />

25<br />

15<br />

15<br />

15<br />

30<br />

60<br />

65<br />

LS<br />

TR<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

NA<br />

TR<br />

TR<br />

TR<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

3<br />

ftA<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

r r r s<br />

OT<br />

HA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA.<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

KA<br />

NA<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

A<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

MATRIX<br />

B/U SD<br />

ST CY COLOR<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U u u u u uuu U<br />

U<br />

U uusssuuu<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y y Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

F<br />

F<br />

F<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

V<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

SD<br />

Y B<br />

Y<br />

GB<br />

Y<br />

B<br />

Y<br />

B<br />

Y B<br />

Y<br />

B<br />

Y B<br />

Y GB<br />

Y<br />

GY<br />

Y GY<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y GE<br />

Y GB<br />

Y Gf<br />

Y GB<br />

Y<br />

GB<br />

Y<br />

GB<br />

Y GB<br />

Y GB<br />

Y<br />

GB<br />

Y<br />

GB<br />

Y GB<br />

Y<br />

GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y<br />

GB<br />

Y GB<br />

Y GB<br />

Y<br />

GB<br />

Y<br />

B<br />

Y<br />

B<br />

Y B<br />

Y<br />

B<br />

Y<br />

B<br />

Y<br />

B<br />

CV<br />

B<br />

GB<br />

GB<br />

B<br />

GB<br />

8B<br />

GB<br />

GB<br />

GY<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

Gf<br />

GP<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

SAND<br />

SAND<br />

SAND<br />

TILL<br />

TILL<br />

TILL


l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l l l<br />

l l<br />

l<br />

l<br />

cobo7apr.wri<br />

TOTAL f OF SAMPLES IN THIS REPORT * 40<br />

SAMPLE<br />

NO.<br />

BOB-87<br />

37-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-IB<br />

-19<br />

-20<br />

-21<br />

-22<br />

-23<br />

38-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

39-01<br />

-02<br />

39-03<br />

WEIGHT (KG.WET)<br />

WEIGHT (GRAMS DRY)<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

H. I. CONC<br />

LABORATORY SAMPLE LOG<br />

AU<br />

DESCRIPTION<br />

sssrssrcsessBrrssrasrsrsssssaccsrs<br />

CLAST<br />

MATRIX<br />

'srsrsrs ssssssssssssssssssx-s<br />

TABLE +10 TABLE TABLE M.I. CONC. NON NO. CALC SIZE l S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL MAG MAG V.G. PPB ssssssssssssssr srsSsa<br />

V/S GR LS OT SD CY<br />

11.0<br />

10.4<br />

10.1<br />

10.2<br />

10.5<br />

10.0<br />

10.6<br />

10.0<br />

10.5<br />

10.7<br />

10.3<br />

11.0<br />

10.7<br />

9.9<br />

8.8<br />

io.a<br />

10.5<br />

10.5<br />

10.4<br />

9.8<br />

9.5<br />

9.6<br />

9.9<br />

10.0<br />

9.5<br />

9.7<br />

10.0<br />

9.5<br />

9.8<br />

10.1<br />

9.6<br />

9.9<br />

7.3<br />

9.9<br />

9.9<br />

10.0<br />

10.1<br />

10.1<br />

9.7<br />

9.7<br />

2.3<br />

1.4<br />

0.5<br />

1.4<br />

1.3<br />

0.4<br />

0.6<br />

0.6<br />

0.7<br />

1.2<br />

1.1<br />

0.5<br />

0.7<br />

0.7<br />

0.3<br />

1.2<br />

1.2<br />

1.0<br />

1.2<br />

0.4<br />

0.5<br />

1.2<br />

1.0<br />

1.2<br />

0.7<br />

0.7<br />

0.9<br />

0.7<br />

1.0<br />

0.8<br />

0.6<br />

0.5<br />

0.5<br />

0.4<br />

0.2<br />

0.0<br />

0.2<br />

0.8<br />

0.8<br />

0.9<br />

8.7<br />

9.0<br />

9.6<br />

8.8<br />

9.2<br />

9.6<br />

10.0<br />

9.4<br />

9.8<br />

9.5<br />

9.2<br />

10.5<br />

10.0<br />

9.2<br />

8.5<br />

9.6<br />

9.3<br />

9.5<br />

9.2<br />

9.4<br />

9.0<br />

8.4<br />

8.9<br />

B.e<br />

8.8<br />

9.0<br />

9.1<br />

8.8<br />

8.8<br />

9.3<br />

9.0<br />

9.4<br />

6.8<br />

9.5<br />

9.7<br />

10.0<br />

9.9<br />

9.3<br />

8.9<br />

8.8<br />

169.9<br />

146.8<br />

161.4<br />

101.5<br />

180.6<br />

142.8<br />

130.3<br />

226.3<br />

144.4<br />

168.7<br />

203.0<br />

120.0<br />

184.0<br />

120.1<br />

120.0<br />

231.3<br />

156.6<br />

170.4<br />

83,0<br />

87.8<br />

191.8<br />

169.8<br />

163.9<br />

148.9<br />

175.9<br />

165.5<br />

181.3<br />

165.7<br />

206.6<br />

208.5<br />

180.3<br />

155.8<br />

173.8<br />

164.4<br />

216.4<br />

166.4<br />

209.5<br />

176.8<br />

169.0<br />

211.3<br />

148.5<br />

120.3<br />

132.6<br />

71.3<br />

148.8<br />

114.3<br />

104.8<br />

182.4<br />

112.5<br />

131.3<br />

166.0<br />

93.8<br />

151.0<br />

94.1<br />

101.4<br />

203.1<br />

130.1<br />

132.3<br />

58.7<br />

70.4<br />

170.4<br />

140.7<br />

132.0<br />

117.2<br />

146.5<br />

140.4<br />

149.2<br />

123.2<br />

177.1<br />

171.9<br />

145.3<br />

127.5<br />

154.6<br />

137.2<br />

193.1<br />

135.7<br />

177.9<br />

140.3<br />

134.2<br />

180.7<br />

21.4<br />

26.5<br />

28.8<br />

30.2<br />

31.8<br />

28.5<br />

25.5<br />

43.9<br />

31.9<br />

37.4<br />

37.0<br />

26.2<br />

33.0<br />

26.0<br />

18.6<br />

28.2<br />

26.5<br />

38.1<br />

24.3<br />

17.4<br />

21.4<br />

29.1<br />

31.9<br />

31.7<br />

29.4<br />

25.1<br />

32.1<br />

42.5<br />

29.5<br />

36.6<br />

35.0<br />

28.3<br />

19.2<br />

27.2<br />

23.3<br />

30.7<br />

31.6<br />

36.5<br />

34.8<br />

30.6<br />

11.8<br />

16.5<br />

17.7<br />

18.0<br />

19.2<br />

17.1<br />

16.7<br />

32.2<br />

21.6<br />

24.6<br />

24.8<br />

16.3<br />

21.7<br />

17.2<br />

12.4<br />

18.3<br />

16.9<br />

24.3<br />

15.5<br />

12.2<br />

14.6<br />

18.2<br />

19.6<br />

20.2<br />

18.6<br />

15.3<br />

20.2<br />

30.4<br />

18.7<br />

23.1<br />

22.2<br />

18.4<br />

12.9<br />

18.6<br />

16.9<br />

23.0<br />

21.0<br />

23.4<br />

23.2<br />

20.2<br />

9.6<br />

10.0<br />

11.1<br />

12.2<br />

12.6<br />

11.4<br />

8.B<br />

11.7<br />

10.3<br />

12.8<br />

12.2<br />

9.9<br />

11.3<br />

8.8<br />

6.2<br />

9.9<br />

9.6<br />

13.8<br />

B.B<br />

5.2<br />

6.6<br />

10.9<br />

12.3<br />

11.5<br />

10.8<br />

9.8<br />

11.9<br />

12.1<br />

10.B<br />

13.5<br />

12.6<br />

9.9<br />

6.3<br />

8.6<br />

6.4<br />

7.7<br />

10.6<br />

13.1<br />

11.6<br />

10.4<br />

0 NA<br />

0 - NA<br />

0 NA<br />

0 NA<br />

1 3553<br />

0 NA<br />

1 2183<br />

1 90<br />

1 134<br />

1 156<br />

0 NA<br />

1 62<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

3 271<br />

1 3631<br />

0 NA<br />

110 7724<br />

159<br />

NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

0 NA<br />

1 143<br />

P<br />

P,C<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P,C<br />

P,C<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P,C<br />

p<br />

P,C<br />

p ppc<br />

TR<br />

C.BL<br />

P<br />

P<br />

P<br />

60<br />

70<br />

80<br />

75<br />

60<br />

BO<br />

60<br />

60<br />

80<br />

60<br />

75<br />

75<br />

80<br />

60<br />

60<br />

60<br />

70<br />

50<br />

50<br />

BS<br />

65<br />

60<br />

65<br />

60<br />

65<br />

69<br />

60<br />

70<br />

70<br />

80<br />

75<br />

80<br />

70<br />

70<br />

50<br />

NA<br />

40<br />

70<br />

60<br />

70<br />

39<br />

30<br />

20<br />

25<br />

20<br />

20<br />

20<br />

20<br />

20<br />

20<br />

25<br />

24<br />

20<br />

20<br />

20<br />

40<br />

30<br />

50<br />

50<br />

15<br />

35<br />

40<br />

34<br />

40<br />

35<br />

30<br />

40<br />

30<br />

30<br />

20<br />

25<br />

20<br />

30<br />

30<br />

50<br />

NA<br />

60<br />

30<br />

40<br />

30<br />

1<br />

NA<br />

NA<br />

NA<br />

NA<br />

TR<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

1<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

1<br />

TR<br />

TR<br />

1<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

KA<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

A<br />

NA<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

HA<br />

NA<br />

A<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

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U<br />

u u<br />

l)<br />

u u u u u u u u u uuuussuuuu<br />

Y<br />

Y<br />

YY<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

F<br />

F<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

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Y<br />

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Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y GB<br />

Y B<br />

Y B<br />

Y B<br />

Y 6B<br />

Y B<br />

Y B<br />

Y GB<br />

Y 6B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y GB<br />

Y GB<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y 66<br />

Y 6B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

B<br />

B<br />

B<br />

B<br />

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69<br />

B<br />

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6B<br />

66<br />

GB<br />

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B<br />

B<br />

GB<br />

GB<br />

6B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

BB<br />

B<br />

B<br />

B<br />

GB<br />

6B<br />

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B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

CLASS<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

SAND<br />

SAND<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

04/


1 111111111111<br />

l<br />

l<br />

PAGE i COGEMA 04,<br />

1<br />

1<br />

1<br />

1<br />

COB08APR.WR1<br />

TOTAL 1 OF SAMPLES IN THIS REPORT = 40<br />

OVERBURDEN DRILLING MANAGEMENT LIHITEO<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION CLA<br />

TABLE<br />

SPLIT<br />

+10<br />

CHIPS<br />

TABLE<br />

FED<br />

TABLE<br />

CONC<br />

M.<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

I. CONC<br />

NON<br />

MAG<br />

NO.<br />

MAG V.G.<br />

CALC SIZE<br />

PPJJ<br />

CLAST<br />

C2SSmi*BW*M*BW*m*<br />

l<br />

rssssrssrsss<br />

V/S GR LS<br />

^^^••^•^••.••••J^^— if^twfm ~if~i—i*^,i<br />

MATRIX<br />

OT<br />

S/USD<br />

ST CY COLIOR<br />

rss<br />

SD<br />

ESS<br />

ESS<br />

CY<br />

BOB-87<br />

39-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

41-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

42-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

43-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

45-01<br />

46-01<br />

-02<br />

47-01<br />

-02<br />

47-03<br />

8.3<br />

9.3<br />

9.9<br />

9.8<br />

9.6<br />

6.8<br />

8.6<br />

7.5<br />

9.9<br />

8.7<br />

8.3<br />

9.4<br />

8.2<br />

10.0<br />

9.7<br />

9.7<br />

6.2<br />

9.6<br />

10.2<br />

10.1<br />

10.1<br />

10.5<br />

10.1<br />

8.2<br />

8.9<br />

10.4<br />

6.4<br />

10.2<br />

10.3<br />

10.5<br />

9.7<br />

10.0<br />

9.6<br />

5.4<br />

10.4<br />

10.0<br />

9.8<br />

9.8<br />

8.5<br />

9.7<br />

0.2<br />

0.4<br />

0.4<br />

0.6<br />

0.8<br />

0.2<br />

0.6<br />

0.8<br />

1.0<br />

0.9<br />

0.8<br />

0.8<br />

0.4<br />

1.5<br />

1.2<br />

1.0<br />

0.5<br />

0.7<br />

0.6<br />

0.6<br />

1.4<br />

1.1<br />

1.4<br />

0.9<br />

0.1<br />

2.0<br />

0.5<br />

1.6<br />

2.2<br />

1.9<br />

0.9<br />

0.4<br />

0.6<br />

0.8<br />

1.1<br />

2.0<br />

0.8<br />

1.0<br />

0.3<br />

0.5<br />

8.1<br />

8.9<br />

9.5<br />

9.2<br />

8.8<br />

6.6<br />

7.8<br />

6.7<br />

8.9<br />

7.8<br />

7.5<br />

8.6<br />

7.8<br />

8.5<br />

6.5<br />

8.7<br />

5.7<br />

8.9<br />

9.4<br />

9.5<br />

8.7<br />

9.4<br />

8.7<br />

7.3<br />

8.8<br />

8.4<br />

5.9<br />

8.4<br />

8.1<br />

8.6<br />

8.6<br />

9.6<br />

9.0<br />

4.6<br />

9.3<br />

8.0<br />

9.0<br />

8.8<br />

8.2<br />

9.2<br />

161.0<br />

88.0<br />

105.1<br />

137.7<br />

107.7<br />

153.5<br />

117.5<br />

79.4<br />

142.5<br />

152.6<br />

90.3<br />

103.7<br />

119.6<br />

140.2<br />

148.3<br />

128.3<br />

112.8<br />

160.2<br />

129.5<br />

168.3<br />

180.3<br />

182.9<br />

161.7<br />

151.0<br />

184.2<br />

232.1<br />

138.1<br />

151.2<br />

179.5<br />

155.1<br />

154.2<br />

125.2<br />

141.4<br />

145.6<br />

210.0<br />

158.4<br />

169.1<br />

140.9<br />

155.8<br />

137.2<br />

133.2 27.8<br />

60.6 27.4<br />

81.2 23.9<br />

111.5 26.2<br />

78.4 29.3<br />

130.0 23.5<br />

97.1 20.4<br />

60.0 19.4<br />

115.8 26.7<br />

128.4 24.2<br />

72.1 18.2<br />

80.9 22.8<br />

96.5 23.1<br />

113.3 26.9<br />

112.6 35.7<br />

94.7 33.6<br />

87.5 25.3<br />

125.4 34.8<br />

99.0 30.5<br />

130.7 37.6<br />

151.0 29.3<br />

152.0 30.9<br />

129.9 31.8<br />

121.9 29.1<br />

151.2 33.0<br />

198.9 33.2<br />

121.0 17.1<br />

128.0 23.2<br />

144.0 35.5<br />

125,8 29.3<br />

121.9 32.3<br />

94.6 30.6<br />

111.7 29.7<br />

123.5 22.1<br />

175.4 34.6<br />

135.5 22.9<br />

141.1 28.0<br />

110.8 30.1<br />

130.6 25.2<br />

119.2 18.0<br />

18.1 9.7<br />

17.5 9.9<br />

15.1 6.8<br />

15.7 10.5<br />

17.2 12.1<br />

15.2 8.3<br />

12.5 7.9<br />

13.6 5.8<br />

17.4 9.3<br />

15.6 6.4<br />

12.2 6.0<br />

15.0 7.8<br />

15.9 7.2<br />

17.4 9.5<br />

23.2 12.5<br />

21.7 11.9<br />

17.8 7.5<br />

23.3 11.5<br />

21.5 9,0<br />

24.0 13.6<br />

17.1 12.2<br />

18.2 12.7<br />

18.6 13.2<br />

16.3 10.8<br />

21.1 11.9<br />

20.6 12.6<br />

11.0 6.1<br />

14.3 8.9<br />

21.1 14.4<br />

18.3 11.0<br />

21.2 11.1<br />

20.1 10.5<br />

18.4 11.3<br />

16.2 5.9<br />

20.3 14.3<br />

12.8 10.1<br />

17.4 10.6<br />

19.5 10.6<br />

16.8 8.4<br />

10.9 7.1<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

2<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

NA P<br />

37 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

220 P<br />

NA P<br />

NA P<br />

NA P<br />

94 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

201 f<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

55 45 NA<br />

70 30 TR<br />

60 40 TR<br />

65 35 TR<br />

60 40 TR<br />

65 35 TR<br />

70 30 TR<br />

80 20 NA<br />

60 40 TR<br />

65 35 NA<br />

70 30 TR<br />

80 20 NA<br />

65 35 NA<br />

60 40 NA<br />

30 70 TR<br />

55 45 NA<br />

45 55 NA<br />

55 45 TR<br />

90 10 NA<br />

60 40 TR<br />

60 40 TR<br />

45 50 5<br />

40 55 5<br />

50 50 TR<br />

60 40 NA<br />

65 30 5<br />

60 35 5<br />

65 35 TR<br />

60 35 5<br />

60 40 TR<br />

60 40 TR<br />

60 40 TR<br />

70 30 NA<br />

60 40 TR<br />

25 75 TR<br />

50 50 TR<br />

20 80 TR<br />

65 35 TR<br />

40 60 TR<br />

50 50 TR<br />

NA U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

A U Y<br />

A U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

A U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y 6B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

6B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL


1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1111111111111<br />

QtsE 1 COGEMA O'<br />

cobo9apr.wri<br />

TOTAL 1 OF SAMPLES IN THIS REPORT 41<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (K6.WET) WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

bin V. ———— — . —— ————— —— ...................H ..........-.^.......•.•.^••••••••"•••"•.•....•••——•••PM*. H——— HHHMM f**,*. -. ——.A.—— MH~ M —— M •.H HI MV BVH MH.XB.Hwa.B —— . W———— ^MB V ——~ V. V. H 1<br />

IIUl<br />

'<br />

TABLE<br />

SPLIT<br />

•no<br />

ruiDc i/nirs<br />

TABLE<br />

FEED<br />

TABLE<br />

CONC<br />

M. I. CONC<br />

M.I. CONC. NON NO.<br />

1 TRUTC TfiTAI MAC MAP 11 C<br />

L * uo i w mini, imu lino Y. D.<br />

CLAST<br />

MATRIX<br />

CALC SIZE l S/U SD ST CY COLOR<br />

r r P "— " *"" •-— ~- — "~ —"<br />

POD ————- . —— —— —— ———— —— ———— —— —— —— —— H-I....K<br />

V/S GR LS OT<br />

SD<br />

CY<br />

BOB-87<br />

47-04<br />

-05<br />

-06<br />

49-01<br />

-02<br />

-03<br />

-04<br />

51-01<br />

-02<br />

52-01<br />

-02<br />

53-01<br />

54-01<br />

-02<br />

-03<br />

55-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

56-01<br />

-02<br />

-03<br />

57-01<br />

-02<br />

58-01<br />

-02<br />

-03<br />

59-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

60-01<br />

-02<br />

-03<br />

-04<br />

61-01<br />

9.3<br />

10.2<br />

9.9<br />

8.1<br />

10.1<br />

10.2<br />

10.0<br />

9.8<br />

9.9<br />

9.6<br />

9.6<br />

10.0<br />

9.9<br />

10.5<br />

7.8<br />

9.9<br />

10.0<br />

9.8<br />

10.0<br />

8.9<br />

10.2<br />

9.1<br />

9.9<br />

10.0<br />

10.3<br />

10.0<br />

7.1<br />

9.8<br />

10.0<br />

9.5<br />

9.6<br />

9.7<br />

9.6<br />

10.1<br />

10.0<br />

9.9<br />

9.6<br />

9.4<br />

10.3<br />

9.7<br />

0.6<br />

0.9<br />

0.9<br />

1.2<br />

2.4<br />

2.0<br />

1.4<br />

1.2<br />

0.6<br />

1.1<br />

0.8<br />

1.4<br />

1.2<br />

3.3<br />

0.6<br />

1.1<br />

0.8<br />

1.2<br />

1.3<br />

1.2<br />

1.3<br />

0.4<br />

2.2<br />

1.7<br />

1.9<br />

0.6<br />

0.3<br />

1.5<br />

1.0<br />

0.6<br />

0.5<br />

1.0<br />

1.3<br />

1.2<br />

1.3<br />

0.5<br />

1.2<br />

0.5<br />

1.3<br />

0.7<br />

6.7<br />

9.3<br />

9.0<br />

6.9<br />

7.7<br />

8.2<br />

8.6<br />

8.6<br />

9.3<br />

8.5<br />

8.6<br />

8.6<br />

8.7<br />

7.2<br />

7.2<br />

8.6<br />

9.2<br />

8.6<br />

8.7<br />

7.7<br />

8.9<br />

8.7<br />

7.7<br />

8.3<br />

8.4<br />

9.4<br />

6.8<br />

8.3<br />

9.0<br />

8.9<br />

9.1<br />

8.7<br />

8.3<br />

8.9<br />

8.7<br />

9.4<br />

8.4<br />

8.9<br />

9.0<br />

9.0<br />

170.0<br />

173.7<br />

200.1<br />

295.1<br />

137.0<br />

233.1<br />

221.8<br />

198.7<br />

155.4<br />

164.2<br />

240.1 -<br />

209.2<br />

276.0<br />

246.6<br />

245.7<br />

228.1<br />

199.0<br />

171.4<br />

264.8<br />

186.0<br />

163.6<br />

178.8<br />

192.7<br />

183.3<br />

324.4<br />

282.5<br />

126.4<br />

171.9<br />

132.0<br />

158.6<br />

144.9<br />

149.0<br />

136.0<br />

162.9<br />

194.9<br />

97.3<br />

111.9<br />

106.8<br />

106.9<br />

132.9<br />

150.4<br />

150.0<br />

173.4<br />

272.0<br />

112.8<br />

207.9<br />

193.1<br />

178.2<br />

128.5<br />

138.4<br />

207.4<br />

173.6<br />

238.0<br />

201.7<br />

213.8<br />

202.0<br />

167.4<br />

139.8<br />

232.3<br />

154.2<br />

127.0<br />

150.4<br />

161.4<br />

145.9<br />

276.2<br />

239.5<br />

98.5<br />

132.5<br />

102.5<br />

126.0<br />

114.7<br />

117.0<br />

97.2<br />

114.0<br />

141.7<br />

71.9<br />

80.7<br />

74.3<br />

74.7<br />

103.5<br />

19.6 11.8<br />

23.7 15.6<br />

26.7 18.4<br />

23.1 15.7<br />

24.2 16.1<br />

25.2 17.0<br />

28.7 19.9<br />

20.5 12.7<br />

26.9 19.1<br />

25.8 15.8<br />

32.7 21.5<br />

35.6 21.8<br />

38.0 26.7<br />

44.9 29.9<br />

31.9 21.6<br />

26.1 15.4<br />

31.6 19.9<br />

31.6 21.1<br />

32.5 20.6<br />

31.8 20.3<br />

36.6 21.1<br />

28.4 18.8<br />

31.3 17.9<br />

37.4 21.8<br />

48.2 25.3<br />

43.0 27.1<br />

27.9 16.8<br />

39.4 22.3<br />

29.5 17.8<br />

32.6 1B.8<br />

30.2 18.1<br />

32,0 20.6<br />

38.8 23.4<br />

48.9 25.9<br />

53.2 28.6<br />

25.4 15.7<br />

31.2 16.6<br />

32.5 20.5<br />

32.2 19.5<br />

29.4 17.7<br />

7.8<br />

8.1<br />

8.3<br />

7.4<br />

8.1<br />

8.2<br />

8.6<br />

7.8<br />

7.8<br />

10.0<br />

11.2.<br />

13.8<br />

11.3<br />

15.0<br />

10.3<br />

10.7<br />

11.7<br />

10.5<br />

11.9<br />

11.5<br />

15.5<br />

9.6<br />

13.4<br />

15.6<br />

22.9<br />

15.9<br />

11.1<br />

17.1<br />

11.7<br />

13.6<br />

12.1<br />

11.4<br />

15.4<br />

23.0<br />

24.6<br />

9.7<br />

12.4<br />

12.0<br />

12.7<br />

11.7<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

1<br />

0<br />

5<br />

1<br />

0<br />

2<br />

5<br />

0<br />

1<br />

0<br />

0<br />

0<br />

11<br />

0<br />

1<br />

0<br />

0<br />

2<br />

0<br />

4<br />

0<br />

NA P 25 75 NA NA U Y<br />

NA P 50 50 TR NA U Y<br />

4 P 60 40 NA A U Y<br />

NA P 10 90 NA NA U Y<br />

NA P 45 55 TR NA U Y<br />

NA P 60 40 NA NA U Y<br />

NA P 90 10 NA NA U Y<br />

NA P,BK 40 50 10 NA U Y<br />

NAP 65 30 5NAUY<br />

NA P 70 30 TR NA U Y<br />

NA P 75 25 TR A U Y<br />

NAP 65 35 TR NA U Y<br />

NA C 90 10 NA A U Y<br />

128 P 60 40 TR NA U Y<br />

528 P 5050TRNAUY<br />

NA P 45 55 NA NA U Y<br />

NA P 30 70 TR NA U Y<br />

NA C 5050NANAUY<br />

303 P 45 54 1 NA U Y<br />

NA C 35 65 NA NA U Y<br />

2639 P 60 40 TR NA U Y<br />

113 P 60 40 TR A U Y<br />

NAP 47 50 3NAUY<br />

566 P 40 60 TR NA U Y<br />

9443 P 90 10 TR NA U Y<br />

NA P 40 60 TR NA S M<br />

126 P 40 60 TR NA S M<br />

NA P 60 40 TR NA U Y<br />

NA P 65 35 TR NA U Y<br />

NA P 60 40 TR NA U Y<br />

1573 P 70 30 NA NA S M<br />

103 C 90 10 TR NA U Y<br />

NA P,C 65 35 TR NA U Y<br />

191 P 40 60 TR NA U Y<br />

NA P 30 65 5 NA U . Y<br />

NA P 20 80 TR NA U Y<br />

416 P 50 50 TR NA U Y<br />

NAP,C 60 39 1 NA U Y<br />

6074 P, C 65 34 1 NA U Y<br />

NA P 60 40 TR NA U Y<br />

Y Y B<br />

Y Y 6B<br />

Y Y GB<br />

Y Y OE<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y OEB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y 6B<br />

Y Y 6B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y N B<br />

Y N B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y N B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

OEB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

6B TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL&BDK<br />

NA SAND<br />

NA SAND<br />

B TILL<br />

B TILL<br />

B TILL<br />

NA SAND<br />

B TILL<br />

6 TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL


1 1 1 1<br />

1<br />

QBE i COGEMA<br />

DDBOAAPR.WRI<br />

TOTAL t OF SAMPLES IN THIS REPORT = 40<br />

1 1111111111111<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

BOB-87<br />

61-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

62-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

63-01<br />

64-01<br />

-02<br />

-03<br />

65-01<br />

-02<br />

-03<br />

-04<br />

66-01<br />

67-01<br />

-02<br />

-03<br />

-05<br />

-06<br />

-07<br />

70-01<br />

-02<br />

72-01<br />

TABLE<br />

Op]<br />

or LI<br />

TTi<br />

PU UrUro I PC<br />

9.9<br />

10.2<br />

9.1<br />

9.1<br />

9.0<br />

9.7<br />

10.0<br />

9.8<br />

10.4<br />

10.2<br />

10.2<br />

10.1<br />

10.0<br />

9.9<br />

9.8<br />

10.1<br />

10.0<br />

9.7<br />

9.8<br />

10.2<br />

10.0<br />

10.3<br />

10.0<br />

9.8<br />

9.6<br />

9.9<br />

10.6<br />

9.5<br />

10.1<br />

10.2<br />

9.0<br />

9.9<br />

8.4<br />

10.2<br />

10.0<br />

9.6<br />

10.0<br />

10.7<br />

5.1<br />

10.1<br />

•HO<br />

0.6<br />

0.9<br />

0.8<br />

0.4<br />

0.5<br />

0.9<br />

1.2<br />

0.7<br />

1.2<br />

1.6<br />

1.5<br />

1.2<br />

0.5<br />

0.4<br />

0.3<br />

0.5<br />

1.0<br />

0.6<br />

1.0<br />

0.3<br />

0.6<br />

0.6<br />

1.2<br />

0.2<br />

1.2<br />

1.0<br />

2.2<br />

1.2<br />

2.6<br />

3.6<br />

0.0<br />

1.8<br />

1.2<br />

1.9<br />

1.8<br />

1.3<br />

1.1<br />

2.0<br />

0.9<br />

0.6<br />

TABLE<br />

FEED<br />

9.3<br />

9.3<br />

8.3<br />

8.7<br />

8.5<br />

8.8<br />

8.6<br />

9.1<br />

9.2<br />

6.6<br />

8.7<br />

8.9<br />

9.5<br />

9.5<br />

9.5<br />

9.6<br />

9.0<br />

9.1<br />

8.6<br />

9.9<br />

9.4<br />

9.7<br />

8.8<br />

9.6<br />

8.4<br />

8.9<br />

8.4<br />

8.3<br />

7.5<br />

6.6<br />

9.0<br />

8.1<br />

7.2<br />

8.3<br />

8.2<br />

8.3<br />

8.9<br />

8.7<br />

4.2<br />

9.5<br />

TABLE<br />

nrvi irv<br />

CONC<br />

91.3<br />

223.4<br />

142.9<br />

183.4<br />

113.9<br />

111.9<br />

73.3<br />

63.6<br />

193.3<br />

312.2<br />

249.1<br />

98.9<br />

84.9<br />

103.6<br />

90.1<br />

91.0<br />

182.6<br />

110.2<br />

193.4<br />

151.4<br />

141.1<br />

158.4<br />

146.3<br />

1151.6<br />

138.3<br />

197.3<br />

166.1<br />

208.9<br />

297.3<br />

217.7<br />

156.7<br />

130.7<br />

92.6<br />

116.5<br />

92.0<br />

106.2<br />

86.4<br />

291.2<br />

341.8<br />

91.8<br />

M.I.<br />

LIGHTS<br />

58.1<br />

187.2<br />

114.4<br />

150.6<br />

86.5<br />

90.0<br />

51.7<br />

39.8<br />

166.6<br />

273.4<br />

207.4<br />

73.4<br />

60.6<br />

71.8<br />

62.8<br />

63.7<br />

139.9<br />

62.5<br />

155.3<br />

117.2<br />

106.1<br />

123.1<br />

114.4<br />

1118.7<br />

105.3<br />

161.0<br />

117.9<br />

179.8<br />

265.7<br />

170.0<br />

131.5<br />

99.2<br />

70.7<br />

90.7<br />

65.7<br />

78.0<br />

63.5<br />

245.9<br />

235.6<br />

65.1<br />

M. I. CWC CLAST MATRIX<br />

srnsssssczsssrss<br />

sssszssssssssssssss szzsssssrrssrssssESas<br />

CONC. NON NO. CALC SIZE l S/U SD ST CY COLOR<br />

TOTAL MAG KfiR u R pc'c —— EZ — ~~~ ~~ c ——<br />

33.2 20.7<br />

36.2 23.5<br />

28.5 16.5<br />

32.8 21.8<br />

27.4 17.4<br />

21.9 12.5<br />

21.6 13.4<br />

23.6 14.9<br />

26.5 15.9<br />

38.6 26.5<br />

41.7 28.6<br />

25.5 15.1<br />

24.3 15.7<br />

31.8 21.2<br />

27.3 17.7<br />

27.3 18.6<br />

42.9 26.3<br />

27.7 17.5<br />

38.1 26.8<br />

34.2 22.9<br />

35.0 23.8<br />

35.3 23.6<br />

31.9 19.6<br />

32.9 24.5<br />

33.0 21.5<br />

36.3 22.9<br />

48.2 30.4<br />

29.1 19.7<br />

31.6 22.9<br />

47.7 32.0<br />

25.2 15.9<br />

31.5 17.8<br />

21.9 13.6<br />

25.6 14.9<br />

26.3 14.5<br />

28.2 16.9<br />

22.9 14.0<br />

45.3 30.3<br />

106.2 100.2<br />

26.7 15.2<br />

i iriu<br />

12.5<br />

12.7<br />

10.0<br />

11.0<br />

10.0<br />

9.4<br />

6.2<br />

8.9<br />

10.6<br />

12.3<br />

13.1<br />

10.4<br />

8.6<br />

10.6<br />

9.6<br />

8.7<br />

16.6<br />

10.2<br />

11.3<br />

11.3<br />

11.2<br />

11.7<br />

12.3<br />

6.4<br />

11.5<br />

13.4<br />

17.8<br />

9.4<br />

8.7<br />

15.7<br />

9.3<br />

13.7<br />

8.3<br />

10.9<br />

11.6<br />

11.3<br />

6.9<br />

15.0<br />

6.0<br />

11.5<br />

i1 9 W*<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

3<br />

1<br />

4<br />

3<br />

0<br />

0<br />

0<br />

0<br />

2<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

1<br />

0<br />

4<br />

2<br />

0<br />

0<br />

0<br />

0<br />

5<br />

0<br />

1<br />

1<br />

1<br />

1<br />

V/S6R<br />

LS<br />

NA P 25 75 NA<br />

NA P 45 49 1<br />

NA P<br />

NAP,6<br />

NA P<br />

NAP.C<br />

NAP.C<br />

NAP,C<br />

397 P, C<br />

144 P<br />

5706 C<br />

284 P<br />

NA P<br />

NA C<br />

NA P<br />

NA P<br />

68 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

6977 P,BL<br />

50 50 50<br />

60 40 NA<br />

60 40 NA<br />

55 45 NA<br />

50 50 NA<br />

60 40 NA<br />

60 40 TR<br />

40 60 NA<br />

50 50 NA<br />

55 45 TR<br />

25 75 TR<br />

50 50 TR<br />

40 60 TR<br />

60 40 TR<br />

65 35 TR<br />

65 35 NA<br />

80 20 TR<br />

75 25 NA<br />

75 25 NA<br />

65 35 TR<br />

65 35 TR<br />

50 40 10<br />

50 50 NA<br />

NAP.BK 90 10 NA<br />

311 P,BL 75 25 TR<br />

NA P 60 35 5<br />

1917 P<br />

210 P<br />

NA TR<br />

NA P<br />

NA P<br />

70 30 TR<br />

70 30 TR<br />

NA NA NA<br />

60 40 TR<br />

30 50 20<br />

NA P 35 60 5<br />

1014 P<br />

NA P<br />

46 P<br />

376 P<br />

4 P<br />

25 P<br />

50 50 TR<br />

60 40 TR<br />

70 30 NA<br />

40 60 TR<br />

60 40 TR<br />

30 70 TR<br />

OT<br />

NA U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

A U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

A U Y<br />

A U Y<br />

NA U Y<br />

NA U Y<br />

NA U Y<br />

SD<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y 6Y<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y BN<br />

Y Y BN<br />

Y Y GB<br />

CY<br />

CLASS<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

BN TILL<br />

BN TILL<br />

GB TILL<br />

04/


^TOE 1<br />

C06EMA<br />

COBOBAPR.WRI<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

TOTAL i OF SAMF1ES IN THIS REFflfiT = 40<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

M. I. CONC<br />

CLAST<br />

MATRIX<br />

CLASS<br />

04,<br />

TABLE<br />

epr TT<br />

ijl L.1 1<br />

+10<br />

LHlra<br />

TABLE<br />

FEED<br />

TABLE<br />

nw UUNU<br />

M.I. CONC. NON<br />

LI Dm 3<br />

1UIHL riMU<br />

NO.<br />

MAR 0 fi<br />

nnu v.o.<br />

CALC SIZE<br />

V/S GR<br />

l<br />

LS OT<br />

S/USD<br />

ST CY<br />

COLOR<br />

SD CY<br />

1 1<br />

1 1<br />

1 1<br />

1<br />

1 1<br />

1 111111111<br />

BOB-87<br />

72-02<br />

-03<br />

73-01<br />

74-01<br />

-02<br />

77-01<br />

-02<br />

78-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

79-01<br />

-02<br />

80-01<br />

82-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

83-01<br />

84-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

85-01<br />

-02<br />

-03<br />

-04<br />

85-05<br />

8.7<br />

6.9<br />

10.1<br />

10.0<br />

9.4<br />

10.0<br />

9.7<br />

9.7<br />

10.0<br />

9.5<br />

9.7<br />

9.0<br />

9.3<br />

9.8<br />

10.0<br />

9.5<br />

9.8<br />

10.0<br />

8.0<br />

8.0<br />

10.2<br />

10.2<br />

10.1<br />

10.1<br />

9.6<br />

9.8<br />

10.7<br />

8.2<br />

9.7<br />

9.4<br />

9.4<br />

9.3<br />

9.1<br />

9.3<br />

9.2<br />

9.4<br />

9.0<br />

8.3<br />

9.6<br />

9.6<br />

0.7<br />

0.5<br />

1.3<br />

1.4<br />

1.0<br />

1.7<br />

1.0<br />

1.4<br />

1.6<br />

1.4<br />

1.0<br />

0.9<br />

1.2<br />

0.8<br />

0.8<br />

1.7<br />

1.5<br />

0.8<br />

0.5<br />

0.8<br />

0.8<br />

0.5<br />

0.3<br />

0.3<br />

0.1<br />

0.8<br />

0.6<br />

0.8<br />

1.0<br />

0.6<br />

1.0<br />

1.3<br />

0.8<br />

0.7<br />

0.6<br />

0.6<br />

0.4<br />

0.6<br />

0.9<br />

0.9<br />

8.0<br />

6.4<br />

8.8<br />

8.6<br />

8.4<br />

8.3<br />

8.7<br />

8.3<br />

8.4<br />

8.1<br />

8.7<br />

8.1<br />

8.1<br />

9.0<br />

9.2<br />

7.8<br />

8.3<br />

9.2<br />

7.5<br />

7.2<br />

9.4<br />

9.7<br />

9.8<br />

9.8<br />

9.5<br />

9.0<br />

9.6<br />

7.4<br />

8.7<br />

8.8<br />

8.4<br />

8.0<br />

8.3<br />

8.6<br />

8.6<br />

8.8<br />

8.6<br />

7.7<br />

8.7<br />

8.7<br />

94.0<br />

89.4<br />

114.5<br />

169.2<br />

99.3<br />

124.2<br />

206.2<br />

146.2<br />

171.9<br />

117.8<br />

185.1<br />

163.2<br />

179.0<br />

191.3<br />

207.6<br />

156.5<br />

195.8<br />

205.7<br />

171.2<br />

136.2<br />

157.4<br />

151.0<br />

187.1<br />

178.2<br />

161.3<br />

191.5<br />

199.1<br />

147.7<br />

157.9<br />

191.9<br />

185.8<br />

184.5<br />

193.6<br />

170.0<br />

195.5<br />

180.4<br />

184.5<br />

227.4<br />

91.2<br />

105.9<br />

69.5<br />

72.8<br />

63.1<br />

135.1<br />

77.8<br />

90.3<br />

179.6<br />

115.2<br />

135.8<br />

87.8<br />

149.7<br />

129.5<br />

132.2<br />

151.4<br />

152.0<br />

121.4<br />

160.7<br />

169.3<br />

132.6<br />

105.1<br />

128.6<br />

121.0<br />

137.6<br />

142.8<br />

131.2<br />

171.0<br />

172.5<br />

118.5<br />

127.6<br />

164.4<br />

165.1<br />

148.6<br />

153.4<br />

135.5<br />

159.7<br />

150.1<br />

154.6<br />

194.6<br />

64.9<br />

81.4<br />

24.5 15.3<br />

16.6 12.2<br />

31.4 17,0<br />

34.1 23.6<br />

21.5 16.1<br />

33.9 20.2<br />

26.6 18.1<br />

31.0 20.8<br />

36.1 24.9<br />

30.0 20.6<br />

35.4 24.0<br />

33.7 23.6<br />

46.8 32.6<br />

39.9 24.6<br />

55.6 37.1<br />

35.1 20.9<br />

35.1 22.1<br />

36.4 24.1<br />

38.6 25.3<br />

31.1 19.2<br />

28.8 18.9<br />

30.0 21.3<br />

49.5 29.5<br />

35.4 22.3<br />

30.1 21.0<br />

20.5 15.6<br />

26.6 17.4<br />

29.2 17.3<br />

30.3 18.7<br />

27.5 17.9<br />

20.7 14.5<br />

35.9 25.1<br />

40.2 28.7<br />

34.5 22.9<br />

35.8 24.9<br />

30.3 19.8<br />

29.9 18.3<br />

32.8 21.2<br />

26.3 17.3<br />

24.5 15.6<br />

9.2<br />

4.4<br />

14.4<br />

10.5<br />

5.4<br />

13.7<br />

8.5<br />

10.2<br />

11.2<br />

9.4<br />

11.4<br />

10.1<br />

14.2<br />

15.1<br />

18.5<br />

14.2<br />

13.0<br />

12.3<br />

13.3<br />

11.9<br />

9.9<br />

8.7<br />

20.0<br />

13.1<br />

9.1<br />

4.9<br />

9.7<br />

11.9<br />

11.6<br />

9.6<br />

6.7<br />

10.8<br />

11.5<br />

11.6<br />

10.9<br />

10.5<br />

11.6<br />

11.6<br />

9.0<br />

8.9<br />

2<br />

1<br />

0<br />

0<br />

1<br />

1<br />

0<br />

0<br />

1<br />

0<br />

0<br />

2<br />

1<br />

0<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

11<br />

4<br />

164 P<br />

123 C<br />

NA C<br />

NA P<br />

587 P<br />

50 P<br />

NA P<br />

NA P<br />

311 P<br />

NA P<br />

NA P<br />

742 P<br />

151 P<br />

NA P<br />

33 F<br />

NA P<br />

NAP,BL<br />

NA P<br />

NA P<br />

NA P<br />

840 P<br />

745 P<br />

NA F<br />

NA F<br />

NA P<br />

NA F<br />

NA P<br />

^ NA P<br />

'C80)P<br />

64 P<br />

.dST)p<br />

197 P<br />

270 P<br />

NA P<br />

NAP,BK<br />

NAP,C<br />

1 fj5r-p r<br />

t VfiV If W<br />

365 P<br />

37 P<br />

339 P<br />

70 25<br />

40 55<br />

10 90<br />

70 30<br />

40 60<br />

60 40<br />

60 40<br />

35 60<br />

35 60<br />

35 60<br />

60 40<br />

50 45<br />

15 70<br />

50 50<br />

20 70<br />

40 60<br />

65 35<br />

40 60<br />

50 45<br />

55 45<br />

65 35<br />

70 30<br />

70 30<br />

65 35<br />

60 40<br />

70 30<br />

75 25<br />

70 30<br />

70 30<br />

40 60<br />

40 60<br />

50 50<br />

65 35<br />

60 40<br />

80 20<br />

60 40<br />

70 30<br />

70 30<br />

70 30<br />

80 20<br />

5 A<br />

5 A<br />

TR NA<br />

TR NA<br />

TR A<br />

TR NA<br />

TR A<br />

5 NA<br />

5 NA<br />

5 NA<br />

TR NA<br />

5 NA<br />

15 A<br />

TR NA<br />

10 NA<br />

TR NA<br />

TR NA<br />

TR NA<br />

5 NA<br />

TR A<br />

NA A<br />

TR A<br />

TR A<br />

TR A<br />

TR A<br />

TR A<br />

TR A<br />

TR NA<br />

TR A<br />

TR NA<br />

TR NA<br />

TR NA<br />

TR NA<br />

TR NA<br />

NA A<br />

TR NA<br />

TR NA<br />

NA NA<br />

TR NA<br />

NA A<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

Y Y GB GB<br />

Y Y GB 6Y<br />

Y Y GB GB<br />

Y Y B B<br />

Y Y GB GY<br />

Y Y GB GB<br />

Y Y B B<br />

Y Y<br />

Y Y<br />

B<br />

B<br />

B<br />

B<br />

Y Y B B<br />

Y Y B B<br />

Y Y GB 68<br />

Y Y B B<br />

Y Y B B<br />

Y Y GB GB<br />

Y Y B B<br />

Y Y B B<br />

Y Y<br />

Y Y<br />

B<br />

B<br />

B<br />

B<br />

Y Y B B<br />

Y Y B B<br />

Y Y<br />

Y Y<br />

6B GB<br />

GB GB<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y<br />

Y Y<br />

Y Y<br />

GB GB<br />

GB GB<br />

GB GB<br />

Y Y<br />

Y Y<br />

B<br />

B<br />

B<br />

B<br />

Y Y B B<br />

Y Y<br />

Y Y<br />

B<br />

B<br />

B<br />

B<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y GB GB<br />

Y Y<br />

Y Y<br />

GB GB<br />

GB GB<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILLttBDK<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


1 1<br />

1 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1 1111111<br />

WE 1<br />

COGEMA<br />

COBOCAPR.WRI . OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

TOTAL if OF SAMPLES IN THIS REPORT = 40<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (K6.WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

lift<br />

NO.<br />

•.••.••.•••.•.••••••. ^ WWW w nB.Bivn~B.MB.^.-.WHH.~~OIM V..v —— —— *.*.H-. —— .|.-. H.I——M—— ~ WHB.M.HM HV WC —— —— ~ ———— M WH. H<br />

BOB-87<br />

85-06<br />

-07<br />

-08<br />

-09<br />

86-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

87-01<br />

-02<br />

-03<br />

88-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

89-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

90-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

90-12<br />

TABLE<br />

SPLIT<br />

10.0<br />

10.0<br />

9.6<br />

9.8<br />

9.0<br />

10.0<br />

10.2<br />

11.0<br />

10.9<br />

10.9<br />

10.3<br />

7.7<br />

10.2<br />

9.8<br />

10.0<br />

6.7<br />

10.5<br />

9.2<br />

7.0<br />

9.6<br />

9.2<br />

9.5<br />

9.8<br />

10.0<br />

10.0<br />

10.0<br />

7.3<br />

9.9<br />

9.8<br />

10.5<br />

9.8<br />

9.3<br />

9.4<br />

9.0<br />

5.3<br />

9.6<br />

7.7<br />

8.8<br />

9.7<br />

9.8<br />

+10<br />

CHIPS<br />

0.6<br />

0.7<br />

0.6<br />

0.7<br />

0.5<br />

0.9<br />

1.5<br />

3.3<br />

2.3<br />

1.1<br />

2.2<br />

0.9<br />

1.4<br />

0.8<br />

0.4<br />

0.3<br />

0.9<br />

0.8<br />

0.4<br />

0.6<br />

0.2<br />

0.8<br />

0.6<br />

.6<br />

.0<br />

.6<br />

.3<br />

.4<br />

.1<br />

2.4<br />

1.6<br />

0.7<br />

1.7<br />

1.1<br />

0.6<br />

1.2<br />

0.6<br />

1.0<br />

0.6<br />

1.0<br />

TABLE<br />

FEED<br />

9.4<br />

9.3<br />

9.0<br />

9.1<br />

8.5<br />

9.1<br />

8.7<br />

7.7<br />

8.6<br />

9.8<br />

6.1<br />

6.8<br />

6.8<br />

9.0<br />

9.6<br />

6.4<br />

9.6<br />

B. 4<br />

6.6<br />

9,0<br />

9.0<br />

8.7<br />

9.2<br />

8.4<br />

9.0<br />

8.4<br />

6.0<br />

8.5<br />

8.7<br />

6.1<br />

8.2<br />

8.6<br />

7.7<br />

7.9<br />

4.7<br />

8.4<br />

7.1<br />

7.8<br />

9.1<br />

8.8<br />

TABLE<br />

CONC<br />

230.4<br />

186.5<br />

160. 6<br />

158.3<br />

140.2<br />

187.9<br />

172.9<br />

174.8<br />

283.5<br />

211.7<br />

127.4<br />

141.1<br />

119.0<br />

81.4<br />

68.0<br />

61.2<br />

106.9<br />

98.3<br />

72.1<br />

112.8<br />

81.7<br />

161.3<br />

206. 1<br />

186.9<br />

225.5<br />

284.4<br />

164.7<br />

253.9<br />

172.4<br />

166.6<br />

179.2<br />

197.2<br />

111.7<br />

201.8<br />

165.4<br />

144.3<br />

90.5<br />

107.7<br />

159.2<br />

126.9<br />

M.<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

196.2<br />

152.1<br />

145.6<br />

118.4<br />

112.4<br />

153.5<br />

138.7<br />

144.1<br />

257.0<br />

180.4<br />

96.9<br />

118.0<br />

86.0<br />

56.7<br />

62.0<br />

41.4<br />

80.0<br />

68.9<br />

51.3<br />

79.2<br />

56.1<br />

134.0<br />

175.2<br />

160.0<br />

190.6<br />

248.7<br />

144.9<br />

206.0<br />

144.9<br />

136.3<br />

146.9<br />

167.9<br />

78.0<br />

170.2<br />

139.4<br />

119.8<br />

71.5<br />

85.3<br />

132.3<br />

97.4<br />

34.2<br />

34.4<br />

35.0<br />

39.9<br />

27.8<br />

34.4<br />

34.2<br />

30.7<br />

26.5<br />

31.3<br />

30.5<br />

23.1<br />

33.0<br />

24.7<br />

26.0<br />

19.8<br />

26.9<br />

29.4<br />

20.8<br />

33.6<br />

25.6<br />

27.3<br />

30.9<br />

26.9<br />

34.9<br />

35.7<br />

19.8<br />

47.9<br />

27.5<br />

30.3<br />

32.3<br />

29.3<br />

33.7<br />

31.6<br />

26.0<br />

24.5<br />

19.0<br />

22.4<br />

26.9<br />

29.5<br />

I. CONC<br />

NON<br />

MAG<br />

23.4<br />

22.8<br />

22.6<br />

26.6<br />

17.0<br />

20.8<br />

20.7<br />

18.0<br />

16.7<br />

19.1<br />

21.0<br />

16.5<br />

18.7<br />

16.1<br />

17.4<br />

12.8<br />

17.4<br />

20.2<br />

13.3<br />

21.3<br />

17.3<br />

17.2<br />

21.3<br />

18.3<br />

24.1<br />

24.2<br />

13.3<br />

33.4<br />

17.2<br />

19.6<br />

19.7<br />

18.2<br />

19.9<br />

19.5<br />

18.9<br />

17.9<br />

12.8<br />

15.7<br />

18.6<br />

20.4<br />

NO.<br />

MAG V.G.<br />

10.8<br />

11.6<br />

12.4<br />

13.1<br />

10.8<br />

13.6<br />

13.5<br />

12.7<br />

9.8<br />

12.2<br />

9.5<br />

6.6<br />

14.3<br />

8.6<br />

6.6<br />

7.0<br />

9.5<br />

9.2<br />

7.5<br />

12.3<br />

6.3<br />

10.1<br />

9.6<br />

8.6<br />

10.6<br />

11.5<br />

6.5<br />

14.5<br />

10.3<br />

10.7<br />

12.6<br />

11.1<br />

13.8<br />

12.1<br />

7.1<br />

6.6<br />

6.2<br />

6.7<br />

8.3<br />

9.1<br />

1<br />

NA P 80 20 NA A U Y Y<br />

142 P 60 40 TR NA U Y Y<br />

CLAST MATRIX<br />

sssssssssssssssssss Esssrsssrs:<br />

CALC SIZE 7. S/U SD ST<br />

V/S GR LS OT<br />

0 NA P 75 25 TR NA U Y Y<br />

1 339 P 60 40 TR NA U Y Y<br />

1 276 P,C 60 39 1 NA U Y Y<br />

NA P,C 70 30 TR NA U Y<br />

455 P,C 60 40 TR A U Y<br />

NA P 70 30 TR NA U Y<br />

NA P, C 70 29 1 NA U Y<br />

Y<br />

YY<br />

Y<br />

346 P,C 70 30 TR NA U Y Y<br />

2749 P,BK 60 20 TR NA U Y Y<br />

NA P,C 70 30 TR NA U Y<br />

368 C 60 20 TR NA U Y<br />

1725 P,BK 80 15 NA NA U Y<br />

Y<br />

Y<br />

Y<br />

608 C 55 45 NA NA U Y Y<br />

226 P 60 40 NA NA U Y Y<br />

396 P 60 40 NA A U Y Y<br />

NA P 60 40 TR A U Y Y<br />

NA P 49 49 2 A U Y Y<br />

NAP,C 60 40 TR A U Y Y<br />

NA P 55 40 5 NA U Y Y<br />

65 P 45 54 1 A U Y Y<br />

NA P 48 48 4 NA U Y Y<br />

640 P,C 60 40 TR HA U Y<br />

47 P 60 40 TR NA U Y<br />

55 P 60 40 NA NA U Y<br />

Y<br />

Y<br />

Y<br />

1698 P,C 70 30 NA NA U Y<br />

NAP.C 60 40 TR NA U Y<br />

Y<br />

Y<br />

NA C 60 40 TR NA U Y Y<br />

NA P,BK 60 20 TR NA U Y Y<br />

0 NAC 5050NANAUY Y<br />

1 2332 C 50 50 NA NA U Y Y<br />

0 NA C 60 40 TR NA U Y Y<br />

0 NA C 60 40 NA NA U Y Y<br />

11 10 C 70 30 NA NA U Y Y<br />

19 C 60 25 15 NA U Y Y<br />

0 NA P 60 40 TR NA U Y Y<br />

0 NA P 80 20 NA NA U Y Y<br />

0 NA P 85 15 NA NA U Y Y<br />

0<br />

0<br />

NAP 6020NAA UY Y<br />

0<br />

1<br />

0<br />

0<br />

1<br />

4<br />

0<br />

1<br />

1<br />

4<br />

3<br />

4<br />

0<br />

0<br />

0<br />

0<br />

2<br />

0<br />

3<br />

1<br />

1<br />

1<br />

0<br />

0<br />

0<br />

sss<br />

CY<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

COLOR<br />

SD CY<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

B B<br />

GB GB<br />

GB GB<br />

B B<br />

GB GB<br />

GB GY<br />

GB GY<br />

GB GY<br />

GB GY<br />

B B<br />

GB GB<br />

B B<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

B B<br />

B B<br />

B B<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

GB GB<br />

CLASS<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

05


1 1<br />

1<br />

1 111111111111111<br />

C06EMA<br />

cobodapr.i wrl<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

TOTAL 1 0! F SAMPLES IN THIS REPORT - 30<br />

LABORATORY SAMPLE LOG<br />

SAMPLE 1 EIGHT (KG. WET) HEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

M. I. CQNC<br />

CLAST<br />

MATRIX<br />

rrz<br />

CLASS<br />

05,<br />

TABLE<br />

SPLIT<br />

+10<br />

PU T r.n<br />

Lnlro<br />

TABLE<br />

FEED<br />

TABLE<br />

M.I. CONC.<br />

1 irUTC TflTAI<br />

LI bm b lumu<br />

NON<br />

MAC<br />

1 Inv<br />

NO.<br />

MAC 1) C<br />

l Inu Y.u.<br />

CALC<br />

DDD rrD<br />

SIZE<br />

V/S GR<br />

X<br />

LS<br />

OT<br />

S/U<br />

SD<br />

ST<br />

CY COLOR<br />

SD<br />

n— —<br />

CY<br />

BOB-87<br />

90-13<br />

-14<br />

91-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

92-01<br />

-02<br />

-03<br />

93-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

94-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

95-01<br />

-02<br />

-03<br />

-04<br />

95-05<br />

9.6<br />

9.6<br />

9.3<br />

8.9<br />

6.6<br />

9.3<br />

8.2<br />

10.0<br />

9.7<br />

10.0<br />

9.2<br />

10.4<br />

7.6<br />

9.3<br />

9.9<br />

10.0<br />

10.2<br />

9.9<br />

9.5<br />

9.4<br />

8.5<br />

9.5<br />

9.5<br />

9.4<br />

9.5<br />

7.7<br />

9.2<br />

9.7<br />

9.3<br />

9.7<br />

1.3<br />

0.8<br />

0.4<br />

0.8<br />

1.0<br />

1.0<br />

0.6<br />

0.8<br />

1.6<br />

1.4<br />

0.5<br />

1.9<br />

0.7<br />

1.1<br />

1.6<br />

2.4<br />

1.6<br />

3.6<br />

1.5<br />

1.0<br />

0.4<br />

0.6<br />

0.9<br />

0.8<br />

1.0<br />

0.7<br />

0.6<br />

1.2<br />

0.9<br />

2.6<br />

8.5<br />

8.8<br />

8.9<br />

8.1<br />

7.8<br />

8.3<br />

7.6<br />

9.2<br />

6.1<br />

8.6<br />

8.7<br />

6.5<br />

6.9<br />

8.2<br />

8.3<br />

7.6<br />

8.6<br />

6.3<br />

8.0<br />

6.4<br />

8.1<br />

8.7<br />

8.6<br />

8.6<br />

8.5<br />

7.0<br />

8.6<br />

8.5<br />

8.4<br />

7.1<br />

139.2<br />

206.4<br />

158.8<br />

185.6<br />

235.7<br />

213.0<br />

234.5<br />

240.6<br />

230. 1<br />

172.2<br />

202.7<br />

179.7<br />

170.4<br />

179,1<br />

227.0<br />

209.5<br />

254.3<br />

208.1<br />

195.1<br />

189.1<br />

163.0<br />

164.9<br />

176.2<br />

166.8<br />

202.0<br />

143.1<br />

189.8<br />

207.7<br />

237.6<br />

294.7<br />

120.7<br />

186.3<br />

133.5<br />

154.6<br />

193.8<br />

177.3<br />

208.2<br />

200.7<br />

175.5<br />

140.1<br />

167.6<br />

14B.O<br />

145.6<br />

147.4<br />

198.9<br />

180.5<br />

212.3<br />

174.2<br />

163.6<br />

157.5<br />

133.1<br />

132.2<br />

146.6<br />

137.0<br />

163.5<br />

117.4<br />

158.1<br />

176.1<br />

207.2<br />

260.9<br />

16.5<br />

20.1<br />

25.3<br />

31.0<br />

41.9<br />

35.7<br />

26.3<br />

39.9<br />

54.6<br />

32.1<br />

35.1<br />

31.7<br />

24.8<br />

31.7<br />

28.1<br />

29.0<br />

42.0<br />

33.9<br />

31.5<br />

31.6<br />

29.9<br />

32.7<br />

29.6<br />

29.8<br />

38.5<br />

25.7<br />

31.7<br />

31.6<br />

30.4<br />

33.8<br />

11.4<br />

13.8<br />

15.9<br />

19.3<br />

24.7<br />

23.6<br />

16.4<br />

26.6<br />

38.6<br />

20.1<br />

21.8<br />

19.8<br />

15.9<br />

20.3<br />

18.6<br />

18.3<br />

26.4<br />

21.8<br />

16.6<br />

19.4<br />

18.9<br />

20.7<br />

18.3<br />

16.8<br />

24.3<br />

15.2<br />

19.3<br />

19.0<br />

18.3<br />

19.8<br />

7.1<br />

6.3<br />

9.4<br />

11.7<br />

17.2<br />

12.1<br />

9.9<br />

13.3<br />

16.0<br />

12.0<br />

13.3<br />

11.9<br />

8.9<br />

11.4<br />

9.5<br />

10.7<br />

15.6<br />

12.1<br />

12.7<br />

12.2<br />

11.0<br />

12.0<br />

11.3<br />

11.0<br />

14.2<br />

10.5<br />

12.4<br />

12.6<br />

12.1<br />

14.0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

1<br />

0<br />

1<br />

0<br />

0<br />

11<br />

0<br />

71<br />

3<br />

01<br />

1<br />

0<br />

0<br />

0<br />

3<br />

0<br />

1<br />

1<br />

1<br />

1<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

43<br />

NA<br />

56<br />

NA<br />

50<br />

NA<br />

NA<br />

467<br />

1796<br />

NA<br />

1092<br />

187<br />

1102<br />

NA<br />

1879<br />

79<br />

NA<br />

m<br />

360<br />

NA<br />

490<br />

152<br />

11<br />

7576<br />

P,C<br />

P<br />

P<br />

P,C<br />

G, P<br />

P<br />

P<br />

P<br />

P,BK<br />

P,C<br />

C<br />

c p<br />

c<br />

c<br />

c cpppppppppp<br />

p p<br />

60<br />

60<br />

60<br />

65<br />

60<br />

50<br />

40<br />

60<br />

70<br />

80<br />

60<br />

60<br />

60<br />

70<br />

70<br />

60<br />

70<br />

70<br />

60<br />

25<br />

25<br />

25<br />

20<br />

25<br />

70<br />

20<br />

20<br />

20<br />

25<br />

60<br />

40<br />

40<br />

40<br />

35<br />

40<br />

50<br />

60<br />

40<br />

30<br />

20<br />

40<br />

40<br />

40<br />

30<br />

30<br />

40<br />

30<br />

30<br />

40<br />

70<br />

70<br />

70<br />

75<br />

70<br />

30<br />

75<br />

75<br />

75<br />

70<br />

35<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

NA<br />

NA<br />

NA<br />

TR<br />

TR<br />

TR<br />

TR<br />

TR<br />

5<br />

5<br />

5<br />

5<br />

5<br />

TR<br />

5<br />

5<br />

5<br />

5<br />

5<br />

NA<br />

NA<br />

A<br />

NA<br />

NA<br />

NA<br />

A<br />

A<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


1<br />

1<br />

1<br />

11111I11111111<br />

m<br />

PAGE i<br />

C06EMA<br />

COfiBjL.WRI<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

TOTAL tt OF SAMPLES IN THIS REPORT = 40<br />

LABORATORY SAMPLE LOG<br />

SAMPLE WEIGHT (KG. WET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

NO.<br />

M. I. CONC<br />

CLAST<br />

MATRIX<br />

CLASS<br />

-*- "- *I—— WH M ———<br />

07/24/67<br />

TABLE<br />

Cpl IT<br />

wTLl 1<br />

+10 TABLE<br />

rut PC ctrn<br />

LHJra rttu<br />

TABLE<br />

nw LUflLf<br />

M.I. CONC. NON<br />

LIGHTS TOTAL MAG<br />

NO.<br />

MAP tl C<br />

nftb Vi b*<br />

CALC SIZE 2 S/U SD<br />

V/S GR LS OT<br />

ST CY COLOR<br />

SD<br />

CY<br />

BOB-87<br />

96-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

97-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

98-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

98-09<br />

8.8<br />

9.0<br />

5.8<br />

9.4<br />

9.0<br />

8.8<br />

8.7<br />

8.8<br />

9.6<br />

8.1<br />

10.2<br />

10.0<br />

9.0<br />

9.8<br />

8.9<br />

9.3<br />

9.9<br />

9.7<br />

9.7<br />

10.1<br />

8.4<br />

9.8<br />

9.7<br />

10.1<br />

9.6<br />

10.4<br />

10.2<br />

9.8<br />

8.9<br />

9.8<br />

8.7<br />

10.0<br />

6.3<br />

9.6<br />

9.8<br />

9.6<br />

8.9<br />

9.5<br />

8.9<br />

9.1<br />

0.6 8.2<br />

0.5 8.5<br />

0.2 5.6<br />

0.4 9.0<br />

0.3 8.7<br />

0.2 8.6<br />

0.4 8.3<br />

0.2 8.6<br />

0.2 9.4<br />

0.2 7.9<br />

0.2 10.0<br />

0.2 9.8<br />

0.2 8.8<br />

0.4 9.4<br />

0.6 8.3<br />

0.2 9.1<br />

0.3 9.6<br />

0.2 9.5<br />

0.4 9.3<br />

0.6 9.5<br />

0.1 8.3<br />

1.0 8.8<br />

0.3 9.4<br />

0.1 10.0<br />

0.0 9.6<br />

0.1 10.3<br />

0.0 10.2<br />

0.0 9.8<br />

0.0 8.9<br />

0.0 9.8<br />

0.2 8.5<br />

0.7 9.3<br />

0.3 8.0<br />

0.5 9.1<br />

0.4 9.4<br />

0.4 9.2<br />

0.2 8.7<br />

0.4 9.1<br />

0.2 8.7<br />

0.2 8.9<br />

138.2<br />

135.4<br />

96.1<br />

143.0<br />

89.8<br />

106.6<br />

144.0<br />

178.8<br />

153.4<br />

192.6<br />

223.1<br />

165.9<br />

154.2<br />

168.7<br />

212.7<br />

160.0<br />

184.7<br />

181.6<br />

133.6<br />

177.0<br />

83.1<br />

189.0<br />

127.0<br />

190.5<br />

155.3<br />

249.8<br />

162.5<br />

173.2<br />

153.0<br />

217.1<br />

156.7<br />

135.8<br />

196.0<br />

212.2<br />

225.3<br />

190.1<br />

173.2<br />

165.8<br />

202.0<br />

187.2<br />

92.0<br />

99.4<br />

71.8<br />

108.6<br />

60.9<br />

77.1<br />

119.2<br />

151.6<br />

123.4<br />

181.6<br />

200.5<br />

131.6<br />

120.7<br />

143.3<br />

191.5<br />

131.6<br />

148.2<br />

157.3<br />

95.7<br />

141.4<br />

50.0<br />

151.8<br />

96.9<br />

161.0<br />

122.6<br />

209.3<br />

122.8<br />

131.6<br />

110.1<br />

172.4<br />

116.1<br />

101.6<br />

158.2<br />

169.1<br />

198.9<br />

154.1<br />

134.5<br />

130.0<br />

182.2<br />

158.3<br />

46.2 32.6<br />

36.0 25.3<br />

24.3 17.4<br />

34.4 23.7<br />

28.9 19.3<br />

29.5 19.8<br />

24.8 17.0<br />

27.2 18.6<br />

30.0 20.0<br />

11.0 7.3<br />

22.6 16.2<br />

34.3 23.0<br />

33.5 23.5<br />

25.4 18.6<br />

21.2 14.0<br />

28.4 21.1<br />

36.5 22.4<br />

24.3 15.8<br />

37.9 24.8<br />

35.6 23.3<br />

33.1 23.2<br />

37.2 25.3<br />

30.1 20.4<br />

29.5 20.3<br />

32.7 22.8<br />

40.5 28.7<br />

39.7 28.B<br />

41.6 29.9<br />

42.9 31.5<br />

44.7 32.2<br />

40.6 30.5<br />

34.2 24.6<br />

37.8 28.3<br />

43.1 31.9<br />

26.4 20.5<br />

36.0 26.0<br />

38.7 28.5<br />

35.8 26.0<br />

19.8 14.2<br />

28.9 20.7<br />

13.6<br />

10.7<br />

6.9<br />

10.7<br />

9.6<br />

9.7<br />

7.8<br />

8.6<br />

10.0<br />

3.7<br />

6.4<br />

11.3<br />

10.0<br />

6.8<br />

7.2<br />

7.3<br />

14.1<br />

8.5<br />

13.1<br />

12.3<br />

9.9<br />

11.9<br />

9.7<br />

9.2<br />

9.9<br />

11.8<br />

10.9<br />

11.7<br />

11.4<br />

12.5<br />

10.1<br />

9.6<br />

9.5<br />

11.2<br />

5.9<br />

10.0<br />

10.2<br />

9.8<br />

5.6<br />

8.2<br />

3<br />

1<br />

0<br />

1<br />

1<br />

1<br />

1<br />

1<br />

0<br />

0<br />

0<br />

2<br />

5<br />

4<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

6<br />

4<br />

0<br />

0<br />

0<br />

0<br />

0<br />

2<br />

1<br />

1<br />

0<br />

63 P 40 40 20 NA U Y<br />

15 P 55 45 NA NA U Y<br />

NAP B020NANAUY<br />

8 P 50 40 10 NA U Y<br />

33 P 60 40 NA NA U Y<br />

10 P 5050NANAUY<br />

22 P 60 40 NA NA U Y<br />

206P 6040NANAUY<br />

NA P 70 30 NA NA U Y<br />

NA P 70 30 NA NA U Y<br />

NAP 5050NANAUY<br />

439 P 60 40 NA NA U Y<br />

186 P 50 50 NA NA U Y<br />

134 P 60 40 NA NA U Y<br />

NA P 70 30 NA NA U Y<br />

9P 7030NANAUY<br />

NA P 50 50 NA NA U Y<br />

NAP 6040NANAUY<br />

NA P 55 45 NA NA U Y<br />

NA P,C 65 35 NA NA U Y<br />

535 P 60 40 NA NA U Y<br />

NA P 60 40 NA NA U Y<br />

NA P 60 40 NA NA U Y<br />

NAP 8020HANAUY<br />

NA TR NA NA NA NA U Y<br />

NA P 75 25 NA NA U Y<br />

396 TR NA NA NA NA U Y<br />

NA TR NA HA NA NA U Y<br />

NA TR NA NA NA NA U Y<br />

89 TR NA NA NA NA U Y<br />

26 P 80 20 NA NA U Y<br />

NA C 8020NANAUY<br />

NA C 75 25 NA NA U Y<br />

NA C 70 30 NA NA U Y<br />

NA C 70 30 NA NA U Y<br />

NA P 75 25 NA NA U Y<br />

534 P 70 30 NA NA U Y<br />

58C 8515NANAUY<br />

6P 7030NANAUY<br />

NAP 7525NANAUY<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y 6B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

6 TILL<br />

B TILL<br />

6 TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL


l l<br />

i<br />

i i<br />

i<br />

i i<br />

i i i i<br />

i i<br />

i<br />

i<br />

i<br />

PAU<br />

cobo2jul.wri<br />

TOTAL t OF SAMPLES IN THIS REPORT = 40<br />

SAfPLE WEIGHT {KG.WET)<br />

NU. :<br />

BOB-87<br />

98-10<br />

-11<br />

-12<br />

99-01<br />

-02<br />

-03<br />

-04<br />

100-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

101-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

101-15<br />

TABLE<br />

BPL I T<br />

8.2<br />

8.9<br />

9.9<br />

9.6<br />

8.2<br />

9.7<br />

9.4<br />

9.2<br />

9.4<br />

9.1<br />

8.9<br />

9.5<br />

9.6<br />

9.9<br />

9.3<br />

9.1<br />

9.8<br />

9.8<br />

7.7<br />

8.1<br />

7.6<br />

9.7<br />

9.5<br />

9.4<br />

10.1<br />

9.7<br />

8.9<br />

10.3<br />

9.5<br />

9.9<br />

10.0<br />

9.3<br />

7.2<br />

9.5<br />

10.0<br />

9.8<br />

9.5<br />

10.0<br />

9.4<br />

8.7<br />

+10<br />

CHIPS<br />

0.2<br />

0.2<br />

0.4<br />

0.3<br />

0.1<br />

0.4<br />

0.4<br />

0.2<br />

0.2<br />

0.0<br />

0.2<br />

0.2<br />

0.2<br />

0.4<br />

0.2<br />

0.2<br />

0.5<br />

0.8<br />

0.2<br />

0.2<br />

0.3<br />

0.3<br />

0.6<br />

0.5<br />

0.8<br />

0.8<br />

0.4<br />

0.7<br />

0.3<br />

0.6<br />

0.5<br />

0.4<br />

0.4<br />

0.4<br />

0.6<br />

0.6<br />

0.2<br />

0.0<br />

0.3<br />

0.5<br />

TABLE<br />

FEED<br />

8.0<br />

8.7<br />

9.5<br />

9.3<br />

8.1<br />

9.3<br />

9.0<br />

9.0<br />

9.2<br />

9.1<br />

8.7<br />

9.3<br />

9.4<br />

9.5<br />

9.1<br />

8.9<br />

9.3<br />

9.0<br />

7.5<br />

7.9<br />

7.3<br />

9.4<br />

8.9<br />

8.9<br />

9.3<br />

8.9<br />

8.5<br />

9.6<br />

9.2<br />

9.3<br />

9.5<br />

8.9<br />

6.8<br />

9.1<br />

9.4<br />

9.2<br />

9.3<br />

10.0<br />

9.1<br />

8.2<br />

TABLE<br />

CONC<br />

218.6<br />

130.5<br />

210.7<br />

149.6<br />

124.8<br />

196.9<br />

134.3<br />

161.8<br />

133.9<br />

153.8<br />

144.9<br />

160.3<br />

207.0<br />

159.7<br />

185.4<br />

109.8<br />

145.4<br />

123.1<br />

142.7<br />

166.8<br />

168.7<br />

251.1<br />

261.1<br />

268.8<br />

289.3<br />

199.3<br />

206.6<br />

365.2<br />

346.1<br />

255.1<br />

273.5<br />

208.4<br />

219.4<br />

185.9<br />

235.7<br />

234.9<br />

231.6<br />

181.5<br />

226.1<br />

170.5<br />

WEIGHT (GRAMS DRY)<br />

M.<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

191.3<br />

97.0<br />

188.4<br />

121.4<br />

106.1<br />

154.3<br />

99.4<br />

131.5<br />

97.4<br />

119.3<br />

109.3<br />

118.8<br />

171.9<br />

123.5<br />

149.6<br />

76.7<br />

112.0<br />

93.0<br />

119.3<br />

135.8<br />

130.6<br />

208.9<br />

209.7<br />

224.2<br />

234.0<br />

175.1<br />

168.6<br />

309.7<br />

291.7<br />

202.7<br />

222.6<br />

168.5<br />

181.9<br />

143.2<br />

194.1<br />

187.4<br />

186.2<br />

138.8<br />

185.8<br />

139.1<br />

27.3<br />

33.5<br />

22,3<br />

28.2<br />

18.7<br />

42.6<br />

34.9<br />

30.3<br />

36.5<br />

34.5<br />

35.6<br />

41.5<br />

35.1<br />

36.2<br />

35.8<br />

33.1<br />

33.4<br />

30.1<br />

23.4<br />

31.0<br />

38.1<br />

42.2<br />

51.4<br />

44.6<br />

55.3<br />

24.2<br />

38.0<br />

55.5<br />

54.4<br />

52.4<br />

50.9<br />

39.9<br />

37.5<br />

42.7<br />

41.6<br />

47.5<br />

45.4<br />

42.7<br />

40.3<br />

31.4<br />

C06EKA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

I. CONC<br />

NON<br />

MAG<br />

19.6<br />

23.4<br />

15.5<br />

20.9<br />

14.2<br />

31.1<br />

25.2<br />

26.3<br />

24.4<br />

22.6<br />

23.3<br />

27.9<br />

23.2<br />

24.1<br />

23.3<br />

22.5<br />

23.7<br />

21.5<br />

16.9<br />

23.4<br />

30.0<br />

33.0<br />

39.5<br />

33.7<br />

41.0<br />

18.7<br />

26.8<br />

39.6<br />

39.6<br />

36.6<br />

36.0<br />

30.1<br />

28.9<br />

30.0<br />

31.1<br />

36.6<br />

34.7<br />

32.2<br />

31.1<br />

23.5<br />

LABORATORY SAMPLE LOG<br />

NO.<br />

MAG V.G.<br />

7.7<br />

10.1<br />

6.8<br />

7.3<br />

4.5<br />

11.5<br />

9.7<br />

4.0<br />

12.1<br />

11.9<br />

12.3<br />

13.6<br />

11.9<br />

12.1<br />

12.5<br />

10.6<br />

9.7<br />

8.6<br />

6.5<br />

7.6<br />

8.1<br />

9.2<br />

11.9<br />

10.9<br />

14.3<br />

5.5<br />

11.2<br />

15.9<br />

14.8<br />

15.8<br />

14.9<br />

9.8<br />

8.6<br />

12.7<br />

10.5<br />

10.9<br />

10.7<br />

10.5<br />

9.2<br />

7.9<br />

1<br />

1<br />

0<br />

0<br />

1<br />

0<br />

6<br />

1<br />

1<br />

1<br />

0<br />

5<br />

6<br />

3<br />

6<br />

0<br />

3<br />

6<br />

2<br />

1<br />

0<br />

1<br />

3<br />

6<br />

5<br />

0<br />

1<br />

1<br />

1<br />

7<br />

5<br />

0<br />

5<br />

3<br />

1<br />

0<br />

1<br />

0<br />

4<br />

0<br />

AU<br />

CLAST<br />

CALC SIZE l<br />

S/U SD<br />

PPB tana.<br />

V/S GR LS OT<br />

19 P<br />

43 P<br />

NA C<br />

NA P<br />

149 P<br />

NA P<br />

112 C<br />

516 P<br />

41 C<br />

17 TR<br />

NA P<br />

86 P<br />

161 C<br />

27 P<br />

I1B P<br />

NA P<br />

136 P<br />

180 P<br />

98 P<br />

91 P<br />

NA P<br />

45 P<br />

108 P<br />

59 P<br />

56 P<br />

NA P<br />

56 C<br />

5 C<br />

16 P<br />

744 P<br />

569 P<br />

NA C<br />

264 C<br />

59 C<br />

93 C<br />

NA C<br />

29 C<br />

NA TR<br />

514 C<br />

m c<br />

75 25<br />

75 25<br />

80 20<br />

40 60<br />

30 70<br />

65 35<br />

80 20<br />

65 35<br />

70 30<br />

m NA<br />

80 20<br />

75 25<br />

80 20<br />

65 35<br />

BO 20<br />

80 20<br />

80 20<br />

85 15<br />

85 15<br />

85 15<br />

95 5<br />

80 20<br />

95 5<br />

85 15<br />

85 15<br />

55 45<br />

50 50<br />

80 20<br />

75 25<br />

80 20<br />

GO 20<br />

70 30<br />

90 10<br />

90 10<br />

95 5<br />

90 10<br />

95 5<br />

NA NA<br />

95 5<br />

80 20<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

m NA.<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA HA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA m<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

3SsrsssssRsssEEsr~~ r<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

MATRIX<br />

STCY COLOR<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

Y Y<br />

SD CY<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

6B<br />

GB<br />

rrr—<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

6 TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

07/27/8}


1 1<br />

1<br />

1 li 11<br />

1<br />

1<br />

1 1111111111<br />

COB03JUL.I ffil<br />

TOTAL 1 Of: SAMPLES IN THIS REPORT = 40<br />

SAMPLE<br />

NO.<br />

60B-87<br />

102-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

103-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

104-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

104-10<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

l SIGHT (KB.HET) WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

TABLE<br />

SPLIT<br />

10.0<br />

9.8<br />

8.8<br />

9.7<br />

10.0<br />

9.9<br />

6.3<br />

9.6<br />

9.3<br />

9.5<br />

10.0<br />

9.2<br />

9.5<br />

9.7<br />

9.6<br />

9.6<br />

9.3<br />

9.7<br />

8.2<br />

9.2<br />

8.7<br />

9.4<br />

9.7<br />

8.3<br />

9.?<br />

9.8<br />

B. 2<br />

8.4<br />

8.2<br />

8.7<br />

7.3<br />

9.3<br />

9.3<br />

9.5<br />

9.4<br />

9.6<br />

9.3<br />

8.6<br />

6.5<br />

10.2<br />

+10<br />

CHIPS<br />

1.6<br />

0.5<br />

0.4<br />

0.7<br />

0.5<br />

0.6<br />

0.2<br />

0.5<br />

0.4<br />

0.4<br />

0.4<br />

0.2<br />

0.4<br />

0.6<br />

0.4<br />

0.6<br />

0.6<br />

0.4<br />

0.4<br />

0.5<br />

0.2<br />

0.7<br />

0.6<br />

0.4<br />

0.4<br />

0.5<br />

0.3<br />

0.5<br />

0.4<br />

0.9<br />

0.2<br />

0.2<br />

0.4<br />

0.4<br />

0.4<br />

0.3<br />

0.4<br />

0.4<br />

0.5<br />

0.4<br />

TABLE<br />

FEED<br />

8.7<br />

9.3<br />

8.4<br />

9.0<br />

9.5<br />

9.3<br />

6.1<br />

9.1<br />

8.9<br />

9.1<br />

9.6<br />

9.0<br />

9.1<br />

9.1<br />

9.2<br />

9.0<br />

8.7<br />

9.3<br />

7.8<br />

8.7<br />

8.5<br />

8.7<br />

9.1<br />

7.9<br />

8.8<br />

9.3<br />

7.9<br />

7.9<br />

7.8<br />

7.8<br />

7.1<br />

9.1<br />

8.9<br />

9.1<br />

9.0<br />

9.3<br />

8.9<br />

B. 7<br />

6.0<br />

9.8<br />

TABLE<br />

CONC<br />

245.5<br />

243.8<br />

236.8<br />

215.8<br />

246.6<br />

209.9<br />

107.4<br />

206.3<br />

199,4<br />

215.2<br />

190.8<br />

164.5<br />

265.0<br />

137.4<br />

149.9<br />

175.4<br />

163.6<br />

160.7<br />

128.9<br />

231.8<br />

109.7<br />

168.6<br />

217.1<br />

154.9<br />

158.4<br />

197.6<br />

192.5<br />

199.8<br />

115.6<br />

140.1<br />

158.4<br />

190.4<br />

221.7<br />

225.1<br />

151.9<br />

229.3<br />

167.8<br />

148.9<br />

145.1<br />

168.0<br />

M. I. CONC<br />

M.I. CONC. NW NO.<br />

LIGHTS TOTAL MAG MAG V.G.<br />

215.7<br />

213.1<br />

207.8<br />

175.9<br />

199.2<br />

160.5<br />

80.9<br />

171.6<br />

162.2<br />

173.3<br />

153.8<br />

125.0<br />

223.7<br />

99.8<br />

113.4<br />

141.2<br />

128.5<br />

136.1<br />

103.7<br />

218.5<br />

95.8<br />

140.2<br />

186.7<br />

119.6<br />

118.3<br />

162.9<br />

167.6<br />

174.0<br />

86.4<br />

105.5<br />

119.9<br />

152.8<br />

187.3<br />

182.4<br />

113.9<br />

187.5<br />

129.8<br />

120.0<br />

118.5<br />

126.6<br />

29.8 19.6<br />

30.7 19.3<br />

29.0 19.9<br />

39.9 25.8<br />

47.4 33.6<br />

49.4 35.6<br />

26.5 20.1<br />

34.7 25.7<br />

37.2 27.3<br />

41.9 30.9<br />

37.0 26.1<br />

39.5 29.6<br />

41.3 30.9<br />

37.6 26.8<br />

36.5 24.7<br />

34.2 23.0<br />

35.1 23.0<br />

24.6 16.8<br />

25.2 16.3<br />

13.3 9.5<br />

13.9 9.2<br />

28.4 19.7<br />

30.4 22.5<br />

35.3 26.0<br />

40.1 25.5<br />

34.7 25.3<br />

24.9 18.3<br />

25.8 18.1<br />

29.2 21.3<br />

34.6 26.7<br />

38.5 26.5<br />

37.6 24.8<br />

34.4 22.8<br />

42.7 28.5<br />

38.0 25.1<br />

41.8 28.2<br />

38.0 26.0<br />

28.9 20.3<br />

26.6 19.6<br />

41.4 29.3<br />

10.0<br />

11.4<br />

9.1<br />

14.1<br />

13.8<br />

13.8<br />

6.4<br />

9.0<br />

9.9<br />

11.0<br />

10.9<br />

9.9<br />

10.4<br />

10.8<br />

11. B<br />

11.2<br />

12.1<br />

7.8<br />

8.9<br />

3.8<br />

4.7<br />

8.7<br />

7.9<br />

9.3<br />

14.6<br />

9.4<br />

6.6<br />

7.7<br />

7.9<br />

7.9<br />

12.0<br />

12.6<br />

11.6<br />

14.2<br />

12.9<br />

13.6<br />

12.0<br />

8.6<br />

7.0<br />

12.1<br />

0<br />

1<br />

1<br />

0<br />

0<br />

6<br />

01<br />

1<br />

0<br />

0<br />

0<br />

0<br />

1<br />

5<br />

4<br />

3<br />

1<br />

i<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

6<br />

7<br />

4<br />

1<br />

0<br />

5<br />

CLAST<br />

CALC SIZE l S/U SD<br />

PPB ^-^-.^<br />

V/S GR LS OT<br />

NA P<br />

1475 P<br />

107 P<br />

NA P<br />

NA C<br />

348 C<br />

NA C<br />

83 C<br />

181 P<br />

NA P<br />

NA P<br />

NA C<br />

NA P<br />

14 P<br />

109 P<br />

888 P<br />

125 P<br />

294 P<br />

235 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

190 P<br />

NA P<br />

NA P<br />

NA C<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

171 C<br />

49 C<br />

69 P<br />

32 P<br />

NA P<br />

104 P<br />

55 45 NA NA U Y<br />

65 35 NA NA U Y<br />

65 35 NA NA U Y<br />

75 25 NA NA U Y<br />

75 25 NA NA U Y<br />

65 15 NA NA U Y<br />

90 10 NA NA U Y<br />

85 15 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

60 20 NA NA U Y<br />

90 10 NA NA U Y<br />

80 20 NA NA U Y<br />

75 25 NA NA U Y<br />

70 30 NA NA U Y<br />

65 35 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

60 20 NA NA U Y<br />

80 20 NA NA U Y<br />

65 15 NA NA U Y<br />

80 20 NA NA U Y<br />

75 25 NA NA U Y<br />

80 20 NA NA U Y<br />

60 20 NA NA U Y<br />

85 15 NA NA U Y<br />

60 40 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

80 20 NA NA U Y<br />

60 20 NA NA U Y<br />

80 20 NA NA U Y<br />

70 30 NA NA U Y<br />

75 25 NA NA U Y<br />

80 20 NA NA U Y<br />

MATRIX<br />

ST CY COLOR<br />

rrrsss<br />

SD CY<br />

CLASS<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y GB<br />

Y Y 6B<br />

Y Y GY<br />

Y Y 6Y<br />

Y Y GB<br />

Y Y GY<br />

Y Y GY<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GY<br />

Y Y GB<br />

Y Y 6B<br />

GB TILL<br />

GB TILL<br />

GY TILL<br />

GY TILL<br />

GB TILL<br />

GY TILL<br />

GY TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GY TILL<br />

GB TILL<br />

GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

Y Y B B TILL<br />

Y Y B 6 TILL<br />

Y Y B B TILL<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GY<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GY TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y B B TILL<br />

07/30/e;


l<br />

l<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

i<br />

CQB04JUL.WRI<br />

TOTAL t OF SAMPLES IN THIS REPORT = 40<br />

COGEMA<br />

OVERBURDEN DRILLINS MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

AU<br />

DESCRIPTION<br />

03/04/8:<br />

CLASS<br />

KU.<br />

'<br />

IB-87<br />

104-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

105-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

106-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

107-01<br />

-02<br />

-03<br />

-04<br />

107-05<br />

TABLE<br />

SPLIT<br />

10.5<br />

10.0<br />

10.4<br />

8.3<br />

10.1<br />

6.6<br />

8.2<br />

9.2<br />

9.4<br />

10.2<br />

9.8<br />

10.6<br />

10.5<br />

9.5<br />

10.4<br />

9.9<br />

8.5<br />

8.6<br />

9.8<br />

10.3<br />

8.9<br />

9.3<br />

7.6<br />

9.3<br />

6.3<br />

10.2<br />

8.9<br />

9.3<br />

8.6<br />

9.9<br />

9.8<br />

9.3<br />

9.4<br />

9.1<br />

9.0<br />

9.6<br />

8.9<br />

9.8<br />

9.5<br />

8.8<br />

•MO<br />

CHIPS<br />

0.5<br />

0.6<br />

0.8<br />

0.4<br />

0.6<br />

0.2<br />

0.6<br />

0.3<br />

0.0<br />

0.2<br />

0.4<br />

0.4<br />

0.7<br />

0.7<br />

0.6<br />

0.5<br />

0.8<br />

0.2<br />

0.4<br />

0.4<br />

0.4<br />

0.5<br />

0.4<br />

0.4<br />

0.2<br />

0.2<br />

0.2<br />

0.3<br />

0.2<br />

0.4<br />

'0.4<br />

0.3<br />

0.4<br />

0.2<br />

0.5<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.5<br />

TABLE<br />

FEED<br />

10.0<br />

9.4<br />

9.6<br />

7.9<br />

9.5<br />

6.4<br />

7.6<br />

8.9<br />

9.4<br />

10.0<br />

9.4<br />

10.2<br />

9.8<br />

8.8<br />

9.8<br />

9.4<br />

7.7<br />

8.4<br />

9.4<br />

9.9<br />

8.5<br />

8.6<br />

7.2<br />

8.9<br />

6.1<br />

10.0<br />

8.7<br />

9.0<br />

8.4<br />

9.5<br />

9.4<br />

9.0<br />

9.0<br />

8.9<br />

8.5<br />

9.5<br />

8.6<br />

9.5<br />

9.1<br />

B. 3<br />

TABLE<br />

CONC<br />

228.5<br />

246.6<br />

254.2<br />

218.6<br />

197.0<br />

90.1<br />

179.5<br />

160.6<br />

186.8<br />

216.2<br />

198.2<br />

214.6<br />

244.0<br />

184.4<br />

223.3<br />

302.8<br />

213.5<br />

144.8<br />

199.9<br />

194.7<br />

134.1<br />

156.6<br />

81.0<br />

112.7<br />

51.2<br />

152.5<br />

154.8<br />

199.9<br />

159.2<br />

208.2<br />

278.1<br />

147.6<br />

173.3<br />

172.3<br />

169.6<br />

194.9<br />

179.3<br />

175.5<br />

134.2<br />

154.7<br />

M.<br />

M.I.<br />

CONC.<br />

LIGHTS TOTAL<br />

201.7<br />

200.0<br />

195.8<br />

176.4<br />

147.5<br />

58.1<br />

145.7<br />

116.0<br />

141.5<br />

167.9<br />

159.6<br />

167.9<br />

203.2<br />

139.4<br />

177.3<br />

254.5<br />

174.1<br />

107.3<br />

162.4<br />

156.4<br />

99.9<br />

123.9<br />

65.3<br />

91.2<br />

38.4<br />

116.8<br />

126.6<br />

174.8<br />

121.0<br />

177.1<br />

235.6<br />

114.3<br />

138.9<br />

135.3<br />

131.0<br />

109.1<br />

136.4<br />

125.3<br />

97.8<br />

122.1<br />

26.6<br />

46.6<br />

58.4<br />

42.2<br />

49.5<br />

32.0<br />

33.6<br />

42.6<br />

45.3<br />

48.3<br />

38.4<br />

46.7<br />

40.6<br />

45.0<br />

46.0<br />

48.3<br />

39.4<br />

37.5<br />

37.5<br />

38.3<br />

34.2<br />

32.7<br />

15.7<br />

21.5<br />

12.8<br />

33.7<br />

28.2<br />

25.1<br />

38.2<br />

31.1<br />

42.5<br />

33.3<br />

34.4<br />

37.0<br />

38.6<br />

85.8<br />

.42.9<br />

50.2<br />

36.4<br />

32.6<br />

i. CONC<br />

NON<br />

MAG<br />

21.4<br />

36.3<br />

44.1<br />

31.9<br />

37.9<br />

25.3<br />

27.6<br />

32,0<br />

36.0<br />

31.1<br />

29.1<br />

33.1<br />

30.5<br />

34.4<br />

33.9<br />

37.3<br />

31.6<br />

27.2<br />

25.9<br />

26.0<br />

21.6<br />

21.5<br />

10.3<br />

14.3<br />

9.2<br />

24.9<br />

20.0<br />

17.6<br />

28.1<br />

22.1<br />

26.8<br />

24.5<br />

25.7<br />

26.8<br />

27.5<br />

39.4<br />

28.0<br />

34.0<br />

25.7<br />

22.0<br />

NO.<br />

MAG V.6.<br />

5.4<br />

10.3<br />

14.3<br />

10.3<br />

11.6<br />

6.7<br />

6.0<br />

10.6<br />

9.3<br />

17.2<br />

9.3<br />

13.6<br />

10.3<br />

10.6<br />

12.1<br />

11.0<br />

7.6<br />

10.3<br />

11.6<br />

12.3<br />

12.6<br />

11.2<br />

5.4<br />

7.2<br />

3.6<br />

8.6<br />

6.2<br />

7.5<br />

10.1<br />

9.0<br />

15.7<br />

8.6<br />

8.7<br />

10.2<br />

11.1<br />

46.4<br />

14.9<br />

16.2<br />

10.7<br />

10.6<br />

0<br />

0<br />

1<br />

3<br />

1<br />

1<br />

0<br />

7<br />

2<br />

4<br />

0<br />

1<br />

0<br />

0<br />

3<br />

3<br />

0<br />

0<br />

1<br />

0<br />

5<br />

4<br />

3<br />

0<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

6<br />

0<br />

0 1 0<br />

0<br />

CALC :<br />

PPB<br />

NA<br />

NA<br />

23<br />

393<br />

1341<br />

40<br />

NA<br />

703<br />

16<br />

1873<br />

NA<br />

31<br />

NA<br />

NA<br />

43<br />

631<br />

NA<br />

NA<br />

14<br />

- NA<br />

87<br />

198<br />

109<br />

NA<br />

NA<br />

60<br />

51<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

149<br />

NA<br />

318<br />

NA<br />

NA<br />

6<br />

NA<br />

NA<br />

szss<br />

SIZE<br />

P<br />

P C p<br />

C<br />

C<br />

P<br />

P<br />

TR<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P<br />

CLAST<br />

7.<br />

5S2SSSSC<br />

V/S GR<br />

60<br />

60<br />

60<br />

75<br />

es<br />

95<br />

75<br />

80<br />

NA<br />

60<br />

70<br />

70<br />

75<br />

65<br />

75<br />

80<br />

80<br />

50<br />

50<br />

40<br />

80<br />

75<br />

70<br />

75<br />

75<br />

60<br />

70<br />

60<br />

70<br />

90<br />

85<br />

90<br />

90<br />

80<br />

75<br />

60<br />

65<br />

60<br />

60<br />

60<br />

40<br />

40<br />

20<br />

25<br />

15<br />

5<br />

25<br />

20<br />

NA<br />

40<br />

30<br />

30<br />

25<br />

35<br />

25<br />

20<br />

20<br />

50<br />

50<br />

60<br />

20<br />

25<br />

30<br />

25<br />

25<br />

20<br />

30<br />

20<br />

30<br />

10<br />

15<br />

10<br />

10<br />

20<br />

25<br />

40<br />

35<br />

40<br />

40<br />

40<br />

LS<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

HA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA m NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

SAI<br />

OT<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

HA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

MATI<br />

SSSS:<br />

SD<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y y Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y Y Y YY Y<br />

Y<br />

Y<br />

Y<br />

RIX<br />

ST<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

CY<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y y Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

COLOR<br />

SD CY<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

B<br />

6<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

6B<br />

B<br />

B<br />

B<br />

B<br />

B<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


l i<br />

i i l<br />

I<br />

i i<br />

l<br />

l i<br />

i l l<br />

l i<br />

i<br />

l<br />

i<br />

PAGEJ<br />

COB01AU6.WRI<br />

TOTAL # CF SAHF1E3 IN THIS REPORT * 40<br />

NU. :<br />

fOB-37<br />

107-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

-21<br />

-22<br />

108-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

109-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

10-9-10<br />

TABLE<br />

SPLIT<br />

9.7<br />

9.5<br />

9.3<br />

9.6<br />

9.6<br />

8.5<br />

9.4<br />

8.9<br />

B. 7<br />

9.1<br />

9.8<br />

9.9<br />

9.9<br />

9.9<br />

9.3<br />

9.4<br />

9.7<br />

9.3<br />

8.9<br />

9.1<br />

9.2<br />

9.7<br />

8. 9<br />

9.1<br />

9.3<br />

9.0<br />

8.8<br />

7.6<br />

9.4<br />

5.2<br />

8.9<br />

9.4<br />

8.9<br />

9.4<br />

10.1<br />

9.9<br />

8.7<br />

10.3<br />

9.6<br />

10.0<br />

•HO<br />

CHIPS<br />

0.3<br />

0.3<br />

0.2<br />

0.4<br />

0.4<br />

0.0<br />

0.0<br />

0.0<br />

0.2<br />

0.2<br />

0.1<br />

3.0<br />

i. 9<br />

0.4<br />

0.4<br />

0.9<br />

0.5<br />

0.7<br />

0.4<br />

0.4<br />

0.3<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.3<br />

0.4<br />

0.4<br />

0.3<br />

0.4<br />

0.3<br />

0.5<br />

0.4<br />

0.2<br />

0.9<br />

0.3<br />

1.4<br />

1.0<br />

0.4<br />

0.6<br />

TABLE<br />

FfB<br />

9.4<br />

9.2<br />

9.1<br />

9.2<br />

9.2<br />

8.5<br />

9.4<br />

8.9<br />

8.5<br />

8.9<br />

9.7<br />

6.9<br />

8.0<br />

9.5<br />

8.9<br />

6.5<br />

9.2<br />

8.6<br />

B. 5<br />

8.7<br />

8.9<br />

9.3<br />

8.5<br />

8.7<br />

8.9<br />

8.7<br />

8.4<br />

7.2<br />

9. J<br />

4.6<br />

8.6<br />

8.9<br />

8,5<br />

9.2<br />

9.2<br />

9.6<br />

7.3<br />

9.3<br />

9.2<br />

9.4<br />

sssssss<br />

TABLE<br />

COHC<br />

138.6<br />

124.3<br />

150. B<br />

157.7<br />

136.1<br />

115.2<br />

141.0<br />

135.8<br />

114.2<br />

150.5<br />

139.3<br />

276.8<br />

246.7<br />

277.4<br />

293.3<br />

175.4<br />

187.0<br />

190.2<br />

197.0<br />

162.4<br />

191.1<br />

210.1<br />

160.0<br />

216.4<br />

182.8<br />

181.2<br />

169.6<br />

148.3<br />

128.8<br />

143.2<br />

186.2<br />

191.4<br />

128.7<br />

180.2<br />

183.3<br />

246.1<br />

219.4<br />

207.6<br />

201.2<br />

161.1<br />

M.I. COHC.<br />

LIGHTS TOTAL<br />

105.7<br />

97.7<br />

115.0<br />

123.6<br />

105.8<br />

90.8<br />

113.7<br />

110.0<br />

90.5<br />

122.7<br />

112.2<br />

244.3<br />

205.6<br />

233.1<br />

232.0<br />

134.3<br />

148.1<br />

141.0<br />

155.9<br />

128.7<br />

154.0<br />

170.0<br />

126.5<br />

179.0<br />

143.8<br />

143.6<br />

134.5<br />

120.5<br />

100.6<br />

128.7<br />

149.8<br />

159.2<br />

95.3<br />

147.0<br />

154.6<br />

220.1<br />

175.4<br />

172.2<br />

169.1<br />

132.5<br />

COGEMA<br />

DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

K. I. COfC CLAST MATRIX<br />

32.9<br />

26.6<br />

35. 6<br />

34.2<br />

30.3<br />

24.4<br />

27.5<br />

25.8<br />

23.7<br />

27.8<br />

27.1<br />

32.0<br />

41.1<br />

44.3<br />

61.3<br />

41.1<br />

38.9<br />

49.2<br />

41.1<br />

33.7<br />

37.1<br />

40.1<br />

33.5<br />

37.4<br />

39.0<br />

37.6<br />

35.1<br />

27.8<br />

28.2<br />

14.5<br />

36". 4<br />

32.2<br />

33.4<br />

33.2<br />

28.7<br />

26.0<br />

44.0<br />

35.4<br />

32.1<br />

28.6<br />

NQN<br />

MAG<br />

21.6<br />

17.4<br />

24.0<br />

22.9<br />

19.9<br />

17.1<br />

18.5<br />

17.4<br />

16.1<br />

20.3<br />

18.1<br />

21.1<br />

28.0<br />

33.9<br />

40.2<br />

29.4<br />

27.2<br />

35.8<br />

30.2<br />

23.0<br />

27.0<br />

27.7<br />

23.9<br />

26.8<br />

27.7<br />

26.0<br />

24.0<br />

19.6<br />

19.1<br />

10.7<br />

24.1<br />

20.4<br />

21.6<br />

19.4<br />

17.8<br />

17.6<br />

28.6<br />

24.5<br />

22.1<br />

20.1<br />

NO.<br />

MAG V.6.<br />

11.3<br />

9.2<br />

11.8<br />

11.2<br />

10.4<br />

7.3<br />

8.8<br />

8.4<br />

7.6<br />

7.5<br />

9.0<br />

10.9<br />

13.1<br />

10.4<br />

21.1<br />

11.7<br />

11.7<br />

13.4<br />

10.9<br />

10.7<br />

10.1<br />

12.4<br />

9.6<br />

10.6<br />

11.3<br />

11.6<br />

11.1<br />

8.2<br />

9.1<br />

3.8<br />

12.3<br />

11.8<br />

11.8<br />

13.8<br />

10.9<br />

8.4<br />

15.4<br />

10.9<br />

10.0<br />

8.5<br />

1<br />

0<br />

6<br />

4<br />

6<br />

1<br />

1<br />

4<br />

1<br />

3<br />

0<br />

1<br />

1<br />

1<br />

1<br />

1<br />

9<br />

4<br />

1<br />

3<br />

6<br />

3<br />

6<br />

6<br />

1<br />

0<br />

4<br />

0<br />

5<br />

0<br />

1<br />

1<br />

5<br />

6<br />

0<br />

1<br />

0<br />

11<br />

0<br />

CALC SIZE<br />

3460 P<br />

NA P<br />

88 P<br />

190 P<br />

109 P<br />

88 TR<br />

35 TR<br />

130 TR<br />

40 P<br />

37 P<br />

NA P<br />

101 P<br />

23 P<br />

44 P<br />

16 p<br />

22 P<br />

211 P<br />

725 P<br />

33 P<br />

75 P<br />

93 P<br />

210 P<br />

181 P<br />

306 P<br />

7 P<br />

NA P<br />

152 P<br />

NA P<br />

306 P<br />

NA P<br />

42 P<br />

18 P<br />

105 P<br />

139 P<br />

NA P<br />

164 P<br />

NA P<br />

26 P<br />

17 P<br />

NA P<br />

V/S GR<br />

X<br />

60 40<br />

75 25<br />

75 25<br />

80 20<br />

75 25<br />

NA RA<br />

NA NA<br />

NA NA<br />

90 10<br />

80 20<br />

80 20<br />

80 20<br />

80 20<br />

80 20<br />

85 15<br />

85 15<br />

80 20<br />

75 25<br />

70 30<br />

70 30<br />

75 25<br />

80 20<br />

70 30<br />

80 20<br />

80 20<br />

90 10<br />

85 15<br />

80 20<br />

70 30<br />

95 5<br />

70 30<br />

80 20<br />

80 20<br />

80 20<br />

70 30<br />

65 35<br />

70 30<br />

65 35<br />

70 30<br />

60 40<br />

LS OT<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

m NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

m NA<br />

NA NA<br />

m NA<br />

NA NA<br />

NA m<br />

m NA<br />

NA NA<br />

NA NA<br />

m NA<br />

NA NA<br />

NA NA<br />

m NA<br />

NA NA<br />

SAI 3D<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

ST CY COd 3ft<br />

SD<br />

CY<br />

Y Y B B FILL<br />

Y Y B b TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

SB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

Y Y B B TILL<br />

Y Y 6B GB TILL<br />

Y Y GB<br />

Y Y GB<br />

GB TILL<br />

GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y GB GB TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y GB GB TILL<br />

Y Y GP GB TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y 6 B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

Y Y B B TILL<br />

08/07/87


l l l l l l<br />

l l l l l l l l l l l<br />

l l<br />

PdGE*<br />

cobo2aug.wri<br />

AoZaus<br />

TOTAL t OF SAMPLES IN THIS REPORT -<br />

SAMPLE<br />

NU. :<br />

BOB-87<br />

109-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

110-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

111-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

- -08<br />

-09<br />

-10<br />

-11<br />

112-01-<br />

-02<br />

-03<br />

.-04<br />

-05<br />

-06<br />

113-01<br />

113-02<br />

WEIGHT (KG.WET)<br />

TABLE<br />

SPLIT<br />

9.6<br />

9.7<br />

9.2<br />

9.6<br />

6.8<br />

8.3<br />

9.5<br />

10.1<br />

9.0<br />

8.9<br />

9.5<br />

8.7<br />

8.8<br />

10.0<br />

9.7<br />

8.6<br />

10.0<br />

9.6<br />

10.4<br />

9.1<br />

3.7<br />

9.9<br />

9.1<br />

9.6<br />

6.6<br />

9.6<br />

7.3<br />

9.5<br />

9.4<br />

8.9<br />

9.5<br />

9.4<br />

9.1<br />

9.0<br />

8.8<br />

9.4<br />

8.9<br />

9.1<br />

6.6<br />

9.6<br />

+10<br />

CHIPS<br />

0.7<br />

0.3<br />

0.3<br />

0.4<br />

0.4<br />

0.6<br />

0.2<br />

0.1<br />

0.4<br />

0.0<br />

0.1<br />

0.3<br />

0.4<br />

0.7<br />

0.8<br />

0.6<br />

0.4<br />

0.6<br />

1.4<br />

1.1<br />

0.4<br />

0.8<br />

0.5<br />

0.6<br />

0.4<br />

0.6<br />

0.4<br />

1.0<br />

0.7<br />

0.4<br />

0.5<br />

0.4<br />

0.8<br />

0.8<br />

1.0<br />

1.1<br />

0.4<br />

0.4<br />

0.3<br />

0.4<br />

TABLE<br />

FEED<br />

8.9<br />

9.4<br />

8.9<br />

9.2<br />

8.4<br />

7.7<br />

9.3<br />

10.0<br />

8.6<br />

8.9<br />

9.4<br />

8.4<br />

8.4<br />

9.3<br />

8.9<br />

8.0<br />

9.6<br />

9.0<br />

9.0<br />

8.0<br />

3.3<br />

9.1<br />

8.6<br />

9.0<br />

8.4<br />

9.0<br />

6.9<br />

8.5<br />

8.7<br />

8.5<br />

9.0<br />

9.0<br />

8.3<br />

8.2<br />

7.8<br />

8.3<br />

8.5<br />

6.7<br />

8.3<br />

9.2<br />

TABLE<br />

CONC<br />

222.0<br />

192.2<br />

235.2<br />

193.6<br />

202.2<br />

178.3<br />

173.7<br />

193.0<br />

165.5<br />

182.6<br />

184.5<br />

248.6<br />

233.0<br />

194.6<br />

217.0<br />

264.6<br />

262.0<br />

275.2<br />

256.0<br />

197.2<br />

99.1<br />

264.3<br />

192.7<br />

222.0<br />

267.7<br />

224.9<br />

171.6<br />

167.3<br />

146.0<br />

194.6<br />

272.4<br />

224.1<br />

231.5<br />

147.8<br />

168.5<br />

209.4<br />

214.7<br />

161.2<br />

182.5<br />

165.7<br />

40<br />

COGEHA<br />

OVERBURDEN DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

M.I. CONC.<br />

LIGHTS TOTAL<br />

184.0<br />

150.5<br />

192.7<br />

156.2<br />

165.0<br />

140.8<br />

131.6<br />

148.2<br />

131.8<br />

118.1<br />

136.3<br />

215.1<br />

211.6<br />

151.9<br />

175.5<br />

216.8<br />

214.6<br />

229.0<br />

172.2<br />

. 159.1<br />

79.8<br />

216.8<br />

147.2<br />

180.7<br />

227.0<br />

192.1<br />

138.5<br />

127.4<br />

108.0<br />

155.6<br />

227.8<br />

156.8<br />

182.3<br />

111.1<br />

122.8<br />

162.9<br />

189.8<br />

128.0<br />

149.5<br />

132.8<br />

^<br />

M. iI. CONC<br />

38.0<br />

41.7<br />

42.5<br />

37.4<br />

37.2<br />

37.5<br />

42.1<br />

44.8<br />

33.7<br />

64.5<br />

48.2<br />

33.5<br />

21.2<br />

42.7<br />

41.5<br />

47.8<br />

47.4<br />

46.2<br />

63.8<br />

36.1<br />

19.3<br />

47.5<br />

45.5<br />

41.3<br />

40.7<br />

32.8<br />

33.1<br />

39.9<br />

40.0<br />

39.0<br />

44.6<br />

67.3<br />

49.2<br />

36.7<br />

45.7<br />

46.5<br />

24.9<br />

33.2<br />

33.0<br />

32.9<br />

rs.'.T; -j.aasj rssrss<br />

NON<br />

MAG<br />

26.2<br />

28.0<br />

30.7<br />

25.9<br />

25.9<br />

27.3<br />

31.0<br />

33.7<br />

24.5<br />

46.7<br />

34.2<br />

24.9<br />

16.4<br />

29.6<br />

28.7<br />

34.8<br />

32.9<br />

28.0<br />

51.5<br />

28.7<br />

14.3<br />

32.3<br />

30.3<br />

27.1<br />

25.9<br />

22,7<br />

22.4<br />

26.7<br />

26.7<br />

25.0<br />

29.4<br />

43.6<br />

34.2<br />

26.1<br />

31.6<br />

32.1<br />

18.7<br />

24.3<br />

22.6<br />

22.3<br />

NO.<br />

MAG V.G.<br />

11.6<br />

13.7<br />

11.8<br />

11.5<br />

11.3<br />

10.2<br />

11.1<br />

11.1<br />

9.2<br />

17.8<br />

14.0<br />

8.6<br />

4.8<br />

13.1<br />

12.8<br />

13.0<br />

14.5<br />

18.2<br />

32.3<br />

9.4<br />

5.0<br />

15.2<br />

15.2<br />

14.2<br />

14.8<br />

10.1<br />

10.7<br />

13.2<br />

13.3<br />

14.0<br />

15.2<br />

23.5<br />

15.0<br />

10.6<br />

14.1<br />

14.4<br />

6.2<br />

8.9<br />

10.4<br />

10.6<br />

0<br />

0<br />

0111<br />

0<br />

152<br />

1<br />

211010<br />

4<br />

6<br />

0<br />

1<br />

1<br />

2<br />

0<br />

0<br />

0<br />

110<br />

0<br />

6<br />

0<br />

1<br />

0<br />

4<br />

4<br />

1<br />

0<br />

0<br />

0<br />

CALC SIZE<br />

PPB<br />

NA P<br />

NA P<br />

NA P<br />

25 P<br />

62 P<br />

14 P<br />

NA P<br />

11 P<br />

154 P<br />

91 TR<br />

144 P<br />

1341 P<br />

39 P<br />

842 P<br />

NA P<br />

142 P<br />

NA P<br />

447 P<br />

168 P<br />

NA P<br />

26 P<br />

46 P<br />

46 P<br />

NA P<br />

NA P<br />

NA P<br />

67 P<br />

38 P<br />

NA P<br />

NA P<br />

83 P<br />

NA P<br />

85 P<br />

NA P<br />

82 P<br />

141 P<br />

34 P<br />

NA P<br />

NA P<br />

NA P<br />

CLAST<br />

^•••.•••.^^^iE5SSSSS !<br />

Z<br />

1V/S6R<br />

55 45<br />

65 35<br />

70 30<br />

75 25<br />

75 25<br />

60 20<br />

60 40<br />

50 50<br />

70 30<br />

NA NA<br />

70 30<br />

60 40<br />

60 40<br />

55 45<br />

50 50<br />

60 40<br />

60 40<br />

65 35<br />

65 35<br />

75 25<br />

85 15<br />

75 25<br />

75 25<br />

75 25<br />

75 25<br />

70 30<br />

70 30<br />

70 30<br />

75 25<br />

75 25<br />

70 30<br />

70 30<br />

70 30<br />

75 25<br />

75 25<br />

75 25<br />

70 30<br />

70 30<br />

65 35<br />

65 35<br />

LS OT<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

HA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

m NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

NA NA<br />

MATRIX<br />

l5/U SD ST CY COLOR<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

U Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y B<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y B<br />

SD CY<br />

CLASS<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

68 TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B<br />

B<br />

TILL<br />

TILL<br />

08/10/87


i i<br />

i i<br />

i<br />

i<br />

i<br />

i<br />

i i<br />

i<br />

i<br />

i i i<br />

i i<br />

i<br />

i<br />

PAfiU<br />

CQB03AU6.WRI<br />

TOTAL l OF SAMPLES IN THIS REPORT = 40<br />

SAMPLE<br />

BOB-87<br />

113-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

114-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

115-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

115-17<br />

WEIGHT (K6.WET)<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

HEIGHT (GRAMS DRY) AU DESCRIPTION<br />

H. I. CONC CLAST MATRIX<br />

TABLE -MO TABLE TABLE M.I. CONC. NON NO. CALC SIZE l S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL MAG MAG V.6. FPB ^^*~~~ essa<br />

V/S GR LS OT SD CY<br />

8.7<br />

8.9<br />

8.1<br />

8.8<br />

9.7<br />

9.1<br />

8.7<br />

9.4<br />

9.2<br />

8.5<br />

8.7<br />

8.6<br />

9.1<br />

9.5<br />

9.4<br />

9.6<br />

9.3<br />

8.4<br />

9.0<br />

8.6<br />

8.7<br />

9.1<br />

9.2<br />

9.2<br />

9.8<br />

9.9<br />

9.7<br />

9.9<br />

9.7<br />

8.9<br />

9.3<br />

9.5<br />

9.2<br />

9.4<br />

9.6<br />

8.2<br />

9.8<br />

9.1<br />

9.0<br />

9.8<br />

0.1<br />

0.8<br />

0.6<br />

1.4<br />

0.6<br />

0.4<br />

0.1<br />

0.8<br />

0.4<br />

0.9<br />

0.6<br />

0.8<br />

0.4<br />

1.0<br />

0.7<br />

0.6<br />

0.4<br />

0.6<br />

1.6<br />

0.8<br />

1.8<br />

1.6<br />

1.4<br />

0.4<br />

0.8<br />

0.8<br />

0.8<br />

0.6<br />

0.8<br />

0.5<br />

0.6<br />

0.7<br />

0.6<br />

0.7<br />

0.7<br />

0.4<br />

0.7<br />

2.1<br />

1.8<br />

2.5<br />

8.6<br />

8.1<br />

7.5<br />

7.4<br />

9.1<br />

8.7<br />

8.6<br />

8.6<br />

6.6<br />

7.6<br />

8.1<br />

7.6<br />

8.7<br />

8.5<br />

8.7<br />

9.0<br />

8.9<br />

7.8<br />

7.4<br />

7.8<br />

6.9<br />

7.5<br />

7.8<br />

8.8<br />

9.0<br />

9.1<br />

8.9<br />

9.3<br />

8.9<br />

6.4<br />

8.7<br />

8.8<br />

8.6<br />

8.7<br />

8.9<br />

7.8<br />

9.1<br />

7.0<br />

7.2<br />

7.3<br />

190.1<br />

225.4<br />

211.0<br />

201.3<br />

202.5<br />

197.7<br />

143.1<br />

195.9<br />

169.5<br />

196.6<br />

250.0<br />

212,4<br />

264.9<br />

219.2<br />

226.2<br />

288.6<br />

213.8<br />

196.4<br />

217.9<br />

246.8<br />

205.4<br />

224.2<br />

262.8<br />

259.2<br />

247.5<br />

230.5<br />

198.4<br />

261.6<br />

190.1<br />

151.5<br />

195.9<br />

202.0<br />

186.3<br />

209.6<br />

242.8<br />

205.6<br />

186.3<br />

156.6<br />

124.9<br />

187.7<br />

142.1<br />

196.1<br />

183.3<br />

163.7<br />

157.3<br />

163.1<br />

112.7<br />

154.0<br />

134.6<br />

168.0<br />

208.7<br />

171.7<br />

219.8<br />

173.0<br />

181.8<br />

236.9<br />

177.0<br />

160.4<br />

1B8.7<br />

190.4<br />

171.3<br />

180.1<br />

220.2<br />

212.7<br />

198.3<br />

181.7<br />

150.7<br />

215.2<br />

149.8<br />

117.5<br />

159.3<br />

168.5<br />

149.7<br />

179.6<br />

207.0<br />

177.6<br />

167.9<br />

117.9<br />

98.9<br />

160.9<br />

48.0 33.6<br />

29.3 20.3<br />

27.7 20.9<br />

37.6 26.3<br />

45.2 31.2<br />

34.6 24.7<br />

30.4 21.9<br />

41.9 28.6<br />

34.9 24.5<br />

28.6 19.5<br />

41.3 30.3<br />

40.7 29.0<br />

45.1 32.3<br />

46.2 33.8<br />

44.4 31.4<br />

51.7 38.5<br />

36.8 26.3<br />

36.0 26.1<br />

29.2 21.0<br />

56.4 34.3<br />

34.1 25.1<br />

44.1 31.4<br />

42.6 29.9<br />

46.5 34.2<br />

49.2 36.5<br />

48.8 36.7<br />

47.7 34.8<br />

46.4 33.4<br />

40.3 27.5<br />

34.0 23.8<br />

36.6 26.3<br />

33.5 23.8<br />

36.6 25.8<br />

30.0 21.2<br />

35.8 26.1<br />

28.0 21.0<br />

18.4 13.7<br />

38.7 26.6<br />

26.0 IB. 8<br />

26.8 20.6<br />

14.4<br />

9.0<br />

6.8<br />

11.3<br />

14.0<br />

9.9<br />

8.5<br />

13.3<br />

10.4<br />

9.1<br />

11.0<br />

11.7<br />

12.8<br />

12.4<br />

13.0<br />

13.2<br />

10.5<br />

9.9<br />

8.2<br />

22.1<br />

9.0<br />

12.7<br />

12.7<br />

12.3<br />

12.7<br />

12.1<br />

12.9<br />

13.0<br />

12.8<br />

10.2<br />

10.3<br />

9.7<br />

10.8<br />

8.8<br />

9.7<br />

7.0<br />

4.7<br />

12.1<br />

7.2<br />

6.2<br />

1<br />

2<br />

0<br />

0<br />

011<br />

0<br />

0<br />

0<br />

41<br />

6<br />

4<br />

1<br />

1<br />

1<br />

1<br />

4<br />

8<br />

3<br />

6<br />

4<br />

0<br />

4<br />

1<br />

1<br />

7<br />

1<br />

0<br />

4<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

2<br />

19 P<br />

486 P<br />

NA P<br />

NA P<br />

NA P<br />

15 P<br />

9 P<br />

HA P<br />

NA P<br />

NA P<br />

53 P<br />

22 P<br />

104 P<br />

215 P<br />

32 P<br />

17 P<br />

145 P<br />

14 P<br />

2561 P<br />

1006 P<br />

794 P<br />

1216 P<br />

202 P<br />

NA P<br />

415 P<br />

17 P<br />

272 P<br />

178 P<br />

55 P<br />

NA P<br />

.-133 P<br />

397 P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

NA P<br />

291 P<br />

NA P<br />

508 P<br />

80 20 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

75 25 NA NA U Y<br />

75 25 NA NA U Y<br />

80 20 NA NA U Y<br />

65 35 NA NA U Y<br />

70 30 NA NA U Y<br />

75 25 NA NA U Y<br />

80 20 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

60 40 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

60-40 NA NA U Y<br />

60 40 NA NA U Y<br />

50 50 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

70 30 NA NA U Y<br />

60 40 NA NA U Y<br />

60 40 NA NA U Y<br />

70 30 NA NA U Y<br />

50 50 NA NA U Y<br />

70 25 5 NA U Y<br />

75 25 NA NA U Y<br />

50 50 NA NA U Y<br />

60 40 NA NA U Y<br />

65 35 NA NA U Y<br />

65 35 NA NA U Y<br />

45 55 NA NA U Y<br />

65 35 NA NA U Y<br />

65 35 NA NA U Y<br />

70 30 NA NA U Y<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y 6B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y 66<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y B<br />

Y Y GB<br />

Y Y GB<br />

Y Y 6B<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y GB<br />

Y Y B<br />

Y Y GB<br />

Y Y 66<br />

Y Y 66<br />

CLASS<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

GB TILL<br />

66 TILL<br />

66 TILL<br />

08/13/87


i<br />

i i i<br />

1<br />

*<br />

1<br />

1<br />

i<br />

i iiiiiii<br />

l i<br />

PAGE l<br />

COB04AUG.HR1<br />

TOTAL l OF SAMPLES IN THIS REPORT =<br />

SAMPLE<br />

NO.<br />

BOB-87<br />

116-01<br />

-02<br />

-03<br />

-04<br />

117-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

118-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

119-01<br />

120-01<br />

121-01<br />

122-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

123-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

124-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

124-06<br />

WEIGHT (KG.WET)<br />

zrrrrr^r^rrrr:<br />

40<br />

COGEMA<br />

OVERBURDEN DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

WEIGHT (GRAMS DRY) AU DESCRIPTION<br />

M. I. CONC CLAST MATRIX<br />

TABLE +10 TABLE TABLE M.I. CONC. NON NO. CALC SIZE X S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL HAG HAG V.G. PPB s——^rrrrrrr rr^r<br />

V/S GR LS OT SD CY<br />

9.3<br />

9.6<br />

9.6<br />

9.5<br />

8.6<br />

9.5<br />

9.8<br />

9.4<br />

10.0<br />

9.1<br />

9.4<br />

9.2<br />

9.1<br />

9.2<br />

9.7<br />

9.6<br />

10.0<br />

9.7<br />

9.6<br />

10.0<br />

10.0<br />

9.8<br />

9.9<br />

9.7<br />

9.6<br />

9.8<br />

10.2<br />

9.3<br />

10.3<br />

9.9<br />

9.6<br />

9.3<br />

9.8<br />

10.2<br />

10.1<br />

9.8<br />

9.8<br />

9.6<br />

9.3<br />

9.6<br />

0.4<br />

0.9<br />

1.2<br />

0.8<br />

0.7<br />

0.9<br />

1.8<br />

1.5<br />

1.0<br />

0.4<br />

0.8<br />

0.8<br />

0.8<br />

0.6<br />

0.8<br />

0.6<br />

0.7<br />

0.8<br />

0.7<br />

0.6<br />

1.0<br />

0.9<br />

1.1<br />

0.4<br />

0.6<br />

0.4<br />

0.3<br />

0.3<br />

0.6<br />

0.3<br />

0.2<br />

0.0<br />

0.4<br />

0.6<br />

0.0<br />

0.5<br />

0.6<br />

0.0<br />

0.0<br />

0.2<br />

8.9<br />

8.7<br />

8.4<br />

8.7<br />

7.9<br />

8.6<br />

8.0<br />

7.9<br />

9.0<br />

8.7<br />

8.6<br />

8.4<br />

8.3<br />

8.6<br />

8.9<br />

9.0<br />

9.3<br />

8.9<br />

6.9<br />

9.4<br />

9.0<br />

8.9<br />

8.8<br />

9.3<br />

9.0<br />

9.4<br />

9.9<br />

9.0<br />

9.7<br />

9.6<br />

9.4<br />

9.3<br />

9.4<br />

9.6<br />

10.1<br />

9.3<br />

9.2<br />

9.6<br />

9.3<br />

9.4<br />

225.1<br />

255.9<br />

219.8<br />

191.6<br />

242.2<br />

232.8<br />

247.7<br />

185.6<br />

190.9<br />

162.7<br />

207.0<br />

182.6<br />

225.4<br />

174.1<br />

241.4<br />

162.3<br />

190.8<br />

188.2<br />

164.4<br />

258.8<br />

207.4<br />

247.6<br />

216.8<br />

216.5<br />

213.1<br />

198.2<br />

296.2<br />

174.1<br />

168.4<br />

253.7<br />

115.6<br />

118.8<br />

188.5<br />

206.6<br />

196.8<br />

165.1<br />

187.8<br />

141.2<br />

137.0<br />

128.5<br />

176.1<br />

194.5<br />

202.4<br />

171.6<br />

218.7<br />

220.6<br />

219.0<br />

167.2<br />

143.8<br />

116.1<br />

160.8<br />

139.1<br />

181.5<br />

136.6<br />

202.6<br />

129.7<br />

144.1<br />

134.6<br />

117.9<br />

207.8<br />

158.1<br />

182.7<br />

163.9<br />

171.4<br />

178.7<br />

154.4<br />

256.4<br />

132.2<br />

126.0<br />

20B.6<br />

71.1<br />

69.5<br />

148.3<br />

178.3<br />

154.7<br />

129.2<br />

151.4<br />

102.4<br />

100.0<br />

101.0<br />

49.0<br />

61.4<br />

17.4<br />

20.0<br />

23.5<br />

12.2<br />

28.7<br />

18.4<br />

47.1<br />

46.6<br />

46.2<br />

43.5<br />

43.9<br />

37.5<br />

38.6<br />

32.6<br />

46.7<br />

53.6<br />

46.5<br />

51.0<br />

49.3<br />

64.9<br />

52.9<br />

45.1<br />

34.4<br />

43.8<br />

39.8<br />

41.9<br />

42.4<br />

45.1<br />

44.5<br />

49.3<br />

40.2<br />

28.3<br />

42.1<br />

35.9<br />

36.4<br />

38.8<br />

37.0<br />

27.5<br />

35.1<br />

45.9<br />

11.3<br />

12.9<br />

15.8<br />

8.1<br />

20.5<br />

13.2<br />

36.8<br />

34.4<br />

33.2<br />

29.7<br />

31.5<br />

26.4<br />

28.8<br />

22.0<br />

33.9<br />

37.7<br />

32.9<br />

36.8<br />

35.2<br />

43.0<br />

35.6<br />

33.1<br />

25.6<br />

31.8<br />

30.8<br />

31.0<br />

29.6<br />

33.6<br />

32.9<br />

37.1<br />

27.9<br />

21.2<br />

30.3<br />

24.3<br />

24.0<br />

27.2<br />

25.7<br />

20.1<br />

13.9<br />

15.5<br />

6.1<br />

7.1<br />

7.7<br />

4.1<br />

8.2<br />

5.2<br />

10.3<br />

12.2<br />

13.0<br />

13.8<br />

12.4<br />

11.1<br />

10.0<br />

10.6<br />

12.8<br />

15.9<br />

13.6<br />

14.2<br />

14.1<br />

21.9<br />

17.3<br />

12.0<br />

8.8<br />

12.0<br />

9.0<br />

10.9<br />

12.8<br />

11.5<br />

11.6<br />

12.2<br />

12.3<br />

7.1<br />

11.8<br />

11.6<br />

12.4<br />

11.6<br />

11.3<br />

7.4<br />

1<br />

2<br />

0<br />

1<br />

4<br />

1<br />

6<br />

0<br />

0<br />

1<br />

0<br />

1<br />

6<br />

1<br />

0<br />

3<br />

3<br />

4<br />

9<br />

1<br />

1<br />

3<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

5<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

0<br />

29<br />

2860<br />

NA<br />

78<br />

161<br />

3077<br />

608<br />

NA<br />

NA<br />

H<br />

NA<br />

34<br />

885<br />

14<br />

NA<br />

122<br />

43<br />

89<br />

138<br />

134<br />

43<br />

21239<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

284<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

TR<br />

P<br />

P<br />

TR<br />

P<br />

P<br />

TR<br />

TR<br />

P<br />

70<br />

70<br />

75<br />

70<br />

70<br />

70<br />

70<br />

70<br />

70<br />

'60<br />

60<br />

60<br />

60<br />

65<br />

65<br />

65<br />

65<br />

70<br />

70<br />

70<br />

70<br />

70<br />

75<br />

70<br />

75<br />

60<br />

60<br />

65<br />

65<br />

60<br />

65<br />

NA<br />

60<br />

65<br />

NA<br />

60<br />

60<br />

NA<br />

NA<br />

60<br />

30 NA<br />

30 NA<br />

25 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

40 NA<br />

40 NA<br />

40 NA<br />

40 NA<br />

35 NA<br />

35 NA<br />

35 NA<br />

35 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

30 NA<br />

25 NA<br />

30 NA<br />

25 NA<br />

40 NA<br />

40 NA<br />

35 NA<br />

35 NA<br />

40 NA<br />

35 NA<br />

NA NA<br />

40 NA<br />

35 NA<br />

NA NA<br />

40 NA<br />

40 NA<br />

NA NA<br />

NA NA<br />

40 NA<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

.NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA U<br />

NA S<br />

NA S<br />

NA U<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

F<br />

F<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

y<br />

Y<br />

y<br />

Y<br />

y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y GB<br />

Y GB<br />

Y 6B<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y GB<br />

Y B<br />

Y B<br />

Y GB<br />

Y B<br />

Y GB<br />

Y GB<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

Y B<br />

CLASS<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

GB TILL<br />

B TILL<br />

GB TILL<br />

GB TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B TILL<br />

B SAND<br />

B SAND<br />

B TILL<br />

08/14/87


l<br />

l<br />

l<br />

l<br />

l<br />

l i<br />

i<br />

l<br />

i<br />

l<br />

l<br />

i<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE l<br />

COB05AU6.HR1<br />

TOTAL t OF SAMPLES IN THIS REPORT = 40<br />

SAMPLE<br />

WEIGHT (KG.WET)<br />

COGEHA<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

M. I. COfC CLAST MATRIX<br />

TABLE +10 TABLE TABLE M.I. CONC. MM NO. CALC SIZE l S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL MAG MAG V.G. FPB ^^*^^^ ^~~<br />

V/S GR LS OT SD CY<br />

BOB-87<br />

124-07<br />

-08<br />

-09<br />

-10<br />

-!1<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

125-01<br />

125A-01<br />

-02<br />

-03<br />

126-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

127-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

128-01<br />

9.7<br />

9.5<br />

9.7<br />

10.0<br />

9.7<br />

9.8<br />

9.1<br />

9.6<br />

10.5<br />

10.6<br />

8.7<br />

9.7<br />

10.0<br />

9.1<br />

9.7<br />

9.4<br />

10.1<br />

9.6<br />

10.9<br />

9.4<br />

9.3<br />

8.7<br />

9.5<br />

9.7<br />

9.8<br />

9.4<br />

9.2<br />

9.2<br />

9.4<br />

9.2<br />

9.6<br />

8.9<br />

8.0<br />

9.3<br />

7.9<br />

9.3<br />

10.8<br />

10.7<br />

9.1<br />

10.8<br />

0.2<br />

0.1<br />

0.4<br />

0.1<br />

0.4<br />

0.2<br />

0.4<br />

0.4<br />

1.4<br />

0.7<br />

0.6<br />

1.9<br />

0.2<br />

0.2<br />

0.6<br />

0.6<br />

0.4<br />

0.2<br />

1.0<br />

0.6<br />

0.4<br />

0.3<br />

0.6<br />

0.2<br />

0.7<br />

0.7<br />

0.2<br />

0.4<br />

0.2<br />

0.2<br />

0.3<br />

0.4<br />

0.0<br />

0.8<br />

0.5<br />

0.6<br />

1.5<br />

1.1<br />

0.8<br />

0.9<br />

9.5<br />

9.4<br />

9.3<br />

9.9<br />

9.3<br />

9.6<br />

8.7<br />

9.2<br />

9.1<br />

9.9<br />

8.1<br />

7.8<br />

9.8<br />

8.9<br />

9.1<br />

8.8<br />

9.7<br />

9.4<br />

9.9<br />

8.8<br />

8.9<br />

8.4<br />

B. 9<br />

9.5<br />

9.1<br />

8.7<br />

9.0<br />

8.8<br />

9.2<br />

9.0<br />

9.3<br />

8.5<br />

8.0<br />

8.5<br />

7.4<br />

8.7<br />

9.3<br />

9.6<br />

8.3<br />

9.9<br />

181.1<br />

128.1<br />

124.6<br />

117.1<br />

136.9<br />

123.1<br />

141.8<br />

145.9<br />

224.0<br />

259.8<br />

164.5<br />

183.8<br />

265.2<br />

193.1<br />

218.6<br />

88.6<br />

219.0<br />

181.3<br />

177.0<br />

164.7<br />

175.4<br />

130.4<br />

173.9<br />

227.3<br />

190.6<br />

152.8<br />

131.9<br />

154.6<br />

170.5<br />

164.0<br />

180.5<br />

159.5<br />

112.3<br />

160.2<br />

125.2<br />

224.4<br />

198.2<br />

200.1<br />

235.2<br />

210.9<br />

155.1<br />

100.7<br />

94.9<br />

92.1<br />

101.6<br />

84.3<br />

111.3<br />

120.3<br />

184.1<br />

213.5<br />

115.3<br />

159.1<br />

237.6<br />

168.5<br />

173.4<br />

54.1<br />

193.7<br />

128.0<br />

142.7<br />

132.2<br />

137.4<br />

91.3<br />

131.8<br />

171.9<br />

149.2<br />

120.3<br />

105.6<br />

112.1<br />

131.6<br />

120.0<br />

147.0<br />

117.5<br />

79.4<br />

127.4<br />

92.1<br />

185.7<br />

152.9<br />

151.0<br />

196.7<br />

165.0<br />

26.0<br />

27.4<br />

29.7<br />

25.0<br />

35.3<br />

38.8<br />

30.5<br />

25.6<br />

39.9<br />

46.3<br />

49.2<br />

24.7<br />

27.6<br />

24.6<br />

45.2<br />

34.5<br />

25.3<br />

53.3<br />

34.3<br />

32.5<br />

38.0<br />

39.1<br />

42.1<br />

55.4<br />

41.4<br />

32.5<br />

26.3<br />

42.5<br />

38.9<br />

44.0<br />

33.5<br />

42.0<br />

32.9<br />

32.8<br />

33.1<br />

38.7<br />

45.3<br />

49.1<br />

38.5<br />

45.9<br />

18.1<br />

19.7<br />

22.7<br />

18.3<br />

25.2<br />

28.7<br />

22.6<br />

18.9<br />

27.7<br />

31.1<br />

33.0<br />

17.9<br />

21.0<br />

19.8<br />

32.5<br />

24.1<br />

18.1<br />

38.0<br />

23.1<br />

23.4<br />

27.3<br />

29.2<br />

31.0<br />

42.0<br />

31.0<br />

23. B<br />

20.9<br />

30.7<br />

29.0<br />

33.9<br />

24.8<br />

32.5<br />

24.5<br />

24.6<br />

23.7<br />

27.7<br />

30.9<br />

34.2<br />

28.5<br />

31.7<br />

7.9<br />

7.7<br />

7.0<br />

6.7<br />

10.1<br />

10.1<br />

7.9<br />

6.7<br />

12.2<br />

15.2<br />

16.2<br />

6.8<br />

6.6<br />

4.8<br />

12.7<br />

10.4<br />

7.2<br />

15.3<br />

11.2<br />

9.1<br />

10.7<br />

9.9<br />

11.1<br />

13.4<br />

10.4<br />

8.7<br />

5.4<br />

11.8<br />

9.9<br />

10.1<br />

8.7<br />

9.5<br />

8.4<br />

8.2<br />

9.4<br />

11.0<br />

14.4<br />

14.9<br />

10.0<br />

14.2<br />

0<br />

0<br />

0<br />

0<br />

0<br />

1<br />

0<br />

0<br />

0<br />

1<br />

3<br />

0<br />

1<br />

1<br />

1<br />

0<br />

1<br />

1<br />

0<br />

0<br />

0<br />

0<br />

0 11 0<br />

0 1 0 1 0<br />

0<br />

0<br />

0<br />

7<br />

0 1 0 1 4<br />

NA<br />

HA<br />

NA<br />

NA<br />

NA<br />

13<br />

NA<br />

NA<br />

NA<br />

915<br />

2725<br />

NA<br />

450<br />

76<br />

65<br />

NA<br />

H<br />

130<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

24<br />

21<br />

NA<br />

NA<br />

252<br />

NA<br />

6<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

94<br />

NA<br />

13<br />

643<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

Tfi<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

P<br />

65<br />

60<br />

70<br />

65<br />

70<br />

70<br />

65<br />

70<br />

70<br />

75<br />

70<br />

70<br />

75<br />

45<br />

60<br />

60<br />

60<br />

90<br />

75<br />

60<br />

60<br />

60<br />

60<br />

60<br />

60<br />

60<br />

40<br />

45<br />

45<br />

50<br />

50<br />

55<br />

NA<br />

60<br />

60<br />

65<br />

65<br />

70<br />

65<br />

65<br />

35<br />

40<br />

30<br />

35<br />

30<br />

30<br />

35<br />

30<br />

30<br />

25<br />

30<br />

30<br />

25<br />

55<br />

40<br />

40<br />

40<br />

10<br />

25<br />

40<br />

40<br />

40<br />

40<br />

40<br />

40<br />

40<br />

60<br />

55<br />

55<br />

50<br />

50<br />

45<br />

NA<br />

40<br />

40<br />

35<br />

35<br />

30<br />

35<br />

35<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

'NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

KA<br />

m<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

B<br />

B<br />

B<br />

6B<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

B<br />

B<br />

B<br />

GB<br />

GB<br />

GB<br />

B<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


1 i<br />

iiiiilr<br />

i iiiiiiiiii<br />

f m. l<br />

*<br />

C0806AU6.WRI<br />

TOTAL i OF SAMF1ES IN THIS REPORT = 50<br />

COGEHA<br />

OVERBURDEN DRILLING MANAGEMENT LIHITED<br />

LABORATORY SAMPLE LOG<br />

08/19/87<br />

CLAST MATRIX<br />

SAMPLE WEIGHT (KE.HET) HEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

NO.<br />

M. I. CGNC<br />

132-01<br />

-02<br />

9.1 0.6 8.5 240.7 208.6 32.1 20.4 11.7 0 RA P 40 60 NA NA U Y Y Y B 6 TILL<br />

9.0 0.6 8.4 209.9 173.5 36.4 23.7 12.7 1 208 P 40 60 NA NA U Y Y Y B B TILL<br />

TABLE +10 TABLE TABLE M.I. CONC. WON NO. CALC SIZE X S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL HAG MAG V.G. PPB<br />

V/S GR LS OT SD CY<br />

BOB-87<br />

128-02 0.9 0.9 0.0 231.6 194.5 37.1 25.8 11.3 1 25 P 70 30 NA NA U Y Y Y GB GB TILL<br />

-03 9.7 0.8 8.9 201.9 154.4 47.5 32.4 15.1 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-04 9.1 0.4 8.7 155.4 105.3 50.1 32.2 17.9 5 199 P 70 30 NA NA U Y Y Y GB GB TILL<br />

-05 9.4 0.3 9.1 177.3 147.6 29.7 21.3 8.4 0 NA P 90 10 NA NA U Y Y Y GB GB TILL<br />

-06 9.8 0.4 9.4 157.6 114.4 43.2 30.3 12.9 0 NA P 80 20 NA NA U Y Y Y GB GB TILL<br />

-07 9.7 0.4 9.3 185.0 139.1 45.9 31.1 14.8 0 NA P 75 25 NA NA U Y Y Y GB GB TILL<br />

-08 9.9 0.8 9.1 226.8 189.7 37.1 25.6 11.5 0 NA P 75 25 NA NA U Y Y Y GB GB TILL<br />

-09 9.5 0.2 9.3 163.8 131.1 32.7 23.4 9.3 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-10 8.8 0.4 8.4 201.5 172.9 28.6 21.7 6.9 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-11 8.9 0.8 8.1 180.0 146.7 33.3 25.6 7.7 0 NA P 70 30 NA NA U Y Y Y GB GB TILL<br />

-12 9.7 0.6 9.1 192.1 154.6 37.5 27.3 10.2 1 283 P 75 25 NA NA U Y Y Y GB GB TILL<br />

-13 9.6 0.9 8.7 210.3 170.9 39.4 28.6 10.8 0 NA BS IS HA NA U Y Y Y GB GB TILL<br />

-14 9.8 0.3 9.5 204.2 170.5 33.7 25.1 8.6 0 m P 75 25 NA NA U Y Y Y GB GB TILL<br />

-15 8.7 0.2 8.5 159.0 130.0 29.0 20.5 8.5 0 NA P 75 25 NA NA U Y Y Y GB GB TILL<br />

-16 10.2 0.5 9.7 215.9 170.5 45.4 34.3 11.1 1 29 P 75 25 NA NA U Y Y Y GB GB TILL<br />

129-01 10.4 0.8 9.6 214.4 168.7 45.7 31.6 14.1 0 NA P 75 25 NA NA U Y Y Y GB GB TILL<br />

-02 9.9 0.6 9.3 174.7 136.9 37.8 27.8 10.0 1 54 P 80 20 NA NA U Y Y Y GB GB TILL<br />

-03 9.1 0.4 8.7 143.9 310.6 33.3 25.2 8.1 0 NA P 80 20 NA NA U Y Y Y GB GB TILL<br />

-04 9.0 0.3 6.7 185.8 153.7 32.1 23.9 8.2 1 670 P 70 30 NA NA U Y Y Y GB GB TILL<br />

-05 9.7 0.2 9.5 177.9 157.2 20.7 14.5 6.2 0 NA P 80 20 NA HA U Y Y Y GB GB TILL<br />

-06 9.6 0.2 9.4 199.5 180.1 19.4 14.3 5.1 0 NA P 70 30 NA NA U Y Y Y GB GB TILL<br />

-07 8.3 0.5 7.fl 142.7 114.7 28.0 21.3 6.7 0 NA P 60 40 NA NA U Y Y Y GB GB TILL<br />

-08 9.7 0.5 9.2 318.5 293.9 24.6 19.0 5.6 1 152 P 60 40 NA NA U Y Y Y GB GB TILL .<br />

-09 10.3 1.1 9.2 304.3 267.9 36.4 24.7 11.7 0 NA P 70 30 NA NA U Y Y Y GB GB TILL<br />

-10 9.7 0.5 9.2 240.2 217.8 22.4 15.6 6.8 6 575 P 60 40 NA NA U Y Y Y GB GB TILL<br />

30-01 10.2 1.4 •8.8 309.5 256.0 53.5 36.8 16.7 1 435 P 60 40 NA NA U Y Y Y GB GB TILL<br />

-02 10.1 0.7 9.4 174.8 133.9 40.9 29.0 11.9. . 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-03 9.7 0.6 9.1 225.3 186.2 39.1 27.1 12.0 0 NA P 60 40 NA NA U Y Y Y GB GB TILL<br />

-04 9.8 0.6 9.2 145.8 111.7 34.1 24.5 9.6 0 NA P 60 40 NA NA U Y Y Y GB GB TILL<br />

-05 9.9 0.8 9.1 154.6 120.7 33.9 24.1 9.8 0 NA P 70 30 NA NA U Y Y Y GB GB TILL<br />

-06 9.0 0.4 8.6 157.8 132.9 24.9 18.2 6.7 1 20 P 65 35 NA NA U Y Y Y GB GB TILL<br />

-07 9.4 0.3 9.1 167.4 137.2 30.2 21.5 8.7 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-08 9.7 0.2 9.5 205.0 170.8 34.2 24.3 9.9 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-09 7.7 0.3 7.4 147.1 122.9 24.2 17.3 6.9 0 NA P 65 35 NA NA U Y Y Y GB GB TILL<br />

-10 9.1 0.6 8.5 207.4 174.5 32.9 23.3 9.6 0 NA P 70 30 NA NA .U Y Y Y GB GB TILL<br />

131-01 9.7 0.5 9.? 253.0 210.7 42.3 28.3 14.0 4 520 P 40 60 NA NA U Y Y Y B B TILL<br />

-02 9.7 0.9 8.8 197.6 150.4 47.2 31.5 15.7 1 3 P 40 60 NA NA U Y Y Y GB GB TILL<br />

-03 9.8 0.6 9.2 183.5 140.4 43.1 28.3 14.6 2 76 P 55 45 NA NA U Y Y Y GB GB TILL<br />

-04 9.6 0.4 9.? 225.8 191.5 34.3 24.0 10.3 1 16 P 70 30 NA NA U Y Y Y GB GB TILL<br />

-05 9.3 0.4 8.9 179.3 142.1 37.2 26.3 10.9 0 NA P 80 20 NA NA U Y Y Y GB GB TILL<br />

-06 9.2 0.4 8.8 216.3 187.3 29.0 19.4 9.6 0 NA P 30 70 NA NA U Y Y Y GB GB TILL<br />

-07 6.8 0.2 8.6 147.2 111.9 35.3 22.8 12.5 0 NA P 40 60 NA NA U Y Y Y GB GB TILL


l ll<br />

l l<br />

PAGE 2 C06EHA 03/19/87<br />

COBQ6AU6.WRI<br />

TOTAL ft OF SAMPLES IN THIS REPORT = . 50<br />

OVERBURDEN DRILLING MANAGEMENT LIMITED<br />

LABORATORY SAMPLE LOG<br />

SAMPLE HEIGHT (KG.WET) WEIGHT (GRAMS DRY) AU DESCRIPTION CLASS<br />

M. I. CONC ' CLAST MATRIX<br />

TABLE +10 TABLE TABLE K.I. CONC. NON NO. CALC SIZE X S/U SD ST CY COLOR<br />

SPLIT CHIPS FEED CONC LIGHTS TOTAL MAS HAG V.6. PPB ^^^z^z~ szrrsr<br />

V/S GR LS OT SD CY<br />

f<br />

1<br />

1<br />

i<br />

i i<br />

i<br />

i i<br />

i<br />

i<br />

i i<br />

i<br />

BOB-87<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

133-01<br />

6.8<br />

9.2<br />

8.7<br />

9.6<br />

9.6<br />

9.6<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

1.0<br />

8.4<br />

B. B<br />

8.3<br />

9.2<br />

9.4<br />

8.6<br />

182.0<br />

174.6<br />

196.8<br />

201.2<br />

209.2<br />

236.6<br />

148.1<br />

137.0<br />

161.7<br />

160.1<br />

170.2<br />

188.9<br />

33.9<br />

37.6<br />

35.1<br />

41.1<br />

39.0<br />

47.7<br />

23.6<br />

24.9<br />

23.8<br />

27.9<br />

27.3<br />

31.8<br />

10.3<br />

12.7<br />

11.3<br />

13.2<br />

11.7<br />

15.9<br />

6<br />

1<br />

1<br />

0<br />

0<br />

1<br />

190<br />

643<br />

2608<br />

NA<br />

NA<br />

12<br />

p<br />

P<br />

P<br />

P<br />

P<br />

P<br />

50<br />

30<br />

30<br />

40<br />

50<br />

50<br />

50<br />

70<br />

70<br />

60<br />

50<br />

50<br />

NA<br />

NA<br />

NA<br />

NA<br />

m<br />

NA<br />

m<br />

NA<br />

m<br />

NA<br />

NA<br />

NA<br />

U<br />

U<br />

U<br />

U<br />

U<br />

U<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

Y<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

GB<br />

6B<br />

GB<br />

GB<br />

GB<br />

GB<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL<br />

TILL


l l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l l l<br />

l<br />

l l<br />

i i<br />

i<br />

i i<br />

PAGE l COGEMA 04/03/87<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNINB<br />

cobolmar.wri<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNIN6S O ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE ft PANNED ^^^ ^--^ ^^^ ^^ MA6 ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

01-01 N 500 X 650 88 C l l<br />

-02 N 150 X 250 38 C l l<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

02-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N 200 X 450 58 C l l<br />

-10 N NO VISIBLE GOLD<br />

03-01 N NO VISIBLE GOLD<br />

l 16.7 11628<br />

l 16.7 683<br />

l 18.0 2539


l l<br />

l l<br />

l<br />

l<br />

l l<br />

l l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l<br />

l<br />

PAGE 2 COGEMA 04/03/87<br />

GOLD CLASSIFICATION<br />

rssssssrrrcrrrrssrs<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobolaar.wri<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNINSS O ———————————-——--——<br />

ABRADED IRREGULAR DELICATE TOTAL NW CALC V.G.<br />

SAMPLE ft PANNED ^^^ ^--^ 8BeE8a:c ~~s MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-87<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

03-05 N NO VISIBLE GOLD


1 1111111111<br />

1 1111111<br />

** COGEMA 03/24/87<br />

GOLD CLASSIFICATION<br />

— ^— _ ^————— ^ WMMV*<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2mar.wri<br />

TOTAL 1 Of PANN<br />

ftAUnJ l" li<br />

SAMPLE 8<br />

PAUMP rHlwHC.<br />

Y/N<br />

irtuO<br />

Z<br />

NUMBER OF GRAINS<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-87<br />

03-06<br />

-07<br />

04-01<br />

-02<br />

-03<br />

-04<br />

05-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

06-01<br />

-02<br />

07-01<br />

-02<br />

-03<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

Y<br />

N<br />

N<br />

N<br />

Y<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

350 X 350 61 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

150 X 200 34 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

1 13.1 4296<br />

1 16.1 4B1<br />

125 X 250 36 C 1 1 EST. 35Z PYRITE<br />

250 X 500 65 C 1 1<br />

100 X 150 25 C 1 1<br />

50 X 100 15 C 1 1<br />

NO VISIBLE GOLD<br />

2 27.0 2877<br />

1 14.6 198<br />

1 16.8 38<br />

100 X 150 25 C 1 l EST. IX PYRITE<br />

150 X 150 29 C 1 1


l l l<br />

l l<br />

l<br />

l l l<br />

l l l<br />

l l l<br />

l<br />

l<br />

l<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEMA 03/24/87<br />

cobo2mar.wri<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNINGS 2 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE ft PANNED ^^^ r^-rrr r^zrrrrr sszrr MAG ASSAY<br />

y/N DIAMETER THICKNESS T P T P T P GMS PPB REHARKS<br />

BOB-87<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N 40() X 400 100 Ml l<br />

08-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

09-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N 75 X 125 20 C l l<br />

-06 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

10-01 N NO VISIBLE GOLD<br />

2 13.5 580<br />

l 16.3 7362<br />

l 20.0 75


l l l<br />

l l<br />

l<br />

l l<br />

l l<br />

l l<br />

l l<br />

l<br />

l<br />

l l<br />

l<br />

PAGA COGEHA 04/03/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND FANNING<br />

COB03MAR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL tt OF RANKINGS 7 ——<br />

ABRADED IRREGULAR DELICATE TOTAL NON<br />

SAMPLE t PANNED<br />

— ^ — —-- ———— ~—— —— ~—— ——— "*—.———.HH. mt*-~——— ilHu<br />

Y/N DIAMETER THICKNESS<br />

P T P T P GMS<br />

BOB-87<br />

10-02<br />

-03<br />

-04<br />

11-01<br />

12-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

N 100 X 150<br />

N<br />

D VISIBLE GOLD<br />

25 X 25<br />

50 X 50<br />

75 X 75<br />

75 X 150<br />

100 X 125<br />

175 X 200<br />

200 X 225<br />

NO VISIBLE GOLD<br />

N 125 X 275<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

Y 25 X 75<br />

50 X 50<br />

75 X 75<br />

75 X 125<br />

125 X 150<br />

100 X 150<br />

250 X 375<br />

275 X 375<br />

25 C l<br />

5C<br />

10 C<br />

15 C<br />

22 C<br />

22 C<br />

36 C<br />

40 C<br />

38C 1 1<br />

l 16.9 171<br />

7 20.5 1373<br />

1 22.9 498<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

EST. 37. PYRITE<br />

10 C 1 EST. 57. PYRITE<br />

10 C 1 307. GARNET<br />

15 C i<br />

20 C 1<br />

27 C 1<br />

25 C 1<br />

56 C 1<br />

58 C 1 1<br />

B 29.4 3260


l l l<br />

l l l<br />

l l l<br />

l l l<br />

l l l l<br />

l l<br />

l<br />

60LD CLASSIFICATION<br />

cssrtirrrszzsszEsrsr<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEHA 04/03/67<br />

COB03MAR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNINGS 7 ——————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE (f PANNED rzrzrsrr ^^:^z rrzrrrrr SZzZr MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

-87<br />

-10<br />

-li<br />

-12<br />

-13<br />

N<br />

Y<br />

Y<br />

Y<br />

-14 N<br />

-15 Y<br />

NO VISIBLE GC<br />

50 X<br />

50 X<br />

25 X<br />

100 X<br />

100 X<br />

125 X<br />

125 X<br />

125 X<br />

150 X<br />

150 X<br />

150 X<br />

150 X<br />

175 X<br />

175 X<br />

200 X<br />

200 X<br />

250 X<br />

250 X<br />

250 X<br />

m x<br />

150 X<br />

250 X<br />

50<br />

75<br />

25<br />

125<br />

250<br />

125<br />

150<br />

175<br />

175<br />

200<br />

225<br />

250<br />

225<br />

250<br />

250<br />

275<br />

250<br />

300<br />

400<br />

200<br />

200<br />

350<br />

200 X 200<br />

75 X<br />

100 X<br />

100 X<br />

150 X<br />

175 X<br />

-16 Y 25 X<br />

50 X<br />

100<br />

125<br />

150<br />

175<br />

175<br />

25<br />

too<br />

10 C<br />

13 C<br />

5C<br />

22 C<br />

34 C<br />

25C<br />

27 C<br />

29 C<br />

31 C<br />

34 C<br />

36 C<br />

38 C<br />

38 C<br />

40 C<br />

42 C<br />

44 C<br />

46 C<br />

50C<br />

58 C<br />

29 C<br />

34 C<br />

54 C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

2<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

38 C l<br />

18 C<br />

22 C<br />

25C<br />

31 C<br />

34 C<br />

5 C<br />

15 C<br />

2<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

2<br />

1<br />

1<br />

1<br />

1<br />

2 24.1<br />

1<br />

2<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

23<br />

19 30.4 7568<br />

3 23.2 2117<br />

l 21.8<br />

3<br />

l<br />

l<br />

l<br />

l<br />

523<br />

7 45.0 489<br />

2<br />

l<br />

EST. 5 1/. PYRITE<br />

10X GARNET<br />

EST. 3 1/. PYRITE<br />

25X GARNET<br />

EST. 0.5X PYRITE<br />

20X GARNET<br />

NO SULPHIDES<br />

307. GARNET<br />

NO SULPHIDES<br />

JOX GARNET


l l l<br />

l l<br />

l<br />

l l<br />

l l l l l l l l l<br />

l<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND FANNING<br />

C06EMA 04/03/87<br />

COB03MAR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL If OF PANNINGS 7 ————————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE # PANNED ^^^ ----. sssssxs SMZS NAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

BOB-87<br />

5Ci X 175 22 C l l<br />

75 X 75 15 C l l<br />

75 X 100 18 C l 2 l 4<br />

100 X 125 22 C l l<br />

100 X 100 20 C l i<br />

125 X 175 29 C 3 l<br />

150 X 250 38 C l l<br />

-17 N 75 X 125 20 C l l<br />

-IB N NO VISIBLE GOLD<br />

-19 N NO VISIBLE GOLD<br />

13-01 N 150 X 250 38 C l l<br />

-02 N 150 X 200 34 C l l<br />

-03 N NO VISIBLE GOLD<br />

14-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

15-01 N NO VISIBLE GOLD<br />

16-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

17-01 N NO VISIBLE GOLD<br />

13 46.3 593<br />

l 16.4 62<br />

l 13.7 632<br />

l 13.9 557


l<br />

m<br />

CDGEMA 04/03/87<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

GOLD aASSIFICATION<br />

sssssrsssrrrsrsrs::::<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB03HAR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL f OF PANNINGS 7 ——————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE K PAWED ^^^ ^^z^ ^^^ s*sss MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-87<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

17-05 N NO VISIBLE GOLD


1<br />

111111111111111111<br />

QE i COGEMA MA<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04MAR. NR1<br />

DAMMIhfTC<br />

TOTAL 1 CF rftNNlNbb 1<br />

NUMBER Of GRAINS<br />

————————————————————————<br />

. . ~ _.~ ~.~ -<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMFtE it PflMUrn ————— —————— ————— ——— MAR flWAV<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

17-06<br />

-07<br />

-OB<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N NO VISIBLE GOLD<br />

N 50 X 75 13 C 1 1<br />

1 16.6 22<br />

-15<br />

-16<br />

-17<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

Y 50 X 100 15 C 1 1 EST. 3V. PYRITE<br />

75 X 75 15 C 1 1<br />

100 X 100 20 C 1 1<br />

3 13.0 214<br />

-16<br />

N 75 X 150 22 C 1 1<br />

1 17.2 123<br />

-19<br />

N 125 l 150 27 C 1 1<br />

1 10.7 358<br />

-20<br />

N<br />

NO VISIBLE GOLD<br />

16-01<br />

N 100 X 150 25 C 1 1<br />

-02<br />

-rn<br />

N<br />

M<br />

NO VISIBLE GOLD<br />

MR VICJFJI F ROi n<br />

1 15.2 190


1<br />

111111111111111111<br />

^GE 2<br />

COGEMA<br />

04,<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04MAR.WRI<br />

NUMBER OF GRAINS<br />

lUIHL f UT rnriNlrfob I —— -~— — —- .— . — — ~ — — —— .-— —<br />

ABRADED IRREGULAR DELICATE TOTAL<br />

i"1 AU CM r~ li r*ifttinn\ *,~.~~. x. ~<br />

SAMPLE B PANNED ssssssss rzrssrrss sssrsssz rrssr<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

NON<br />

KAR<br />

twVJ<br />

6MS<br />

CALC V.G,<br />

A^AY<br />

nudn i<br />

PPB<br />

BOB-87<br />

-04 N NO VISIBLE GOLD<br />

-05 N 100 X 125 22 C 1 1<br />

1<br />

15.7 135<br />

19-01 N 75 X 150 22 C 1 i<br />

1<br />

12.6 166<br />

-02 N NO VISIBLE GOLD<br />

-03 N 200 X 250 42 C 1 1<br />

1<br />

16.0 1001<br />

-04 N NO VISIBLE GOLD<br />

-05 N 100 X 150 25 C 1 1<br />

1<br />

19.3 150<br />

-06 N NO VISIBLE GOLD<br />

20-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N 100 X 100 20 CI '1<br />

1<br />

29.9 50<br />

-06 N 100 X 100 20 C 1 1<br />

1<br />

27.6 54<br />

-07 N 200 X 400 54 C 1 1<br />

1<br />

25.6 1424<br />

-08 N NO VISIBLE GOLD


l<br />

l<br />

l l<br />

l l<br />

l l l l<br />

l l l<br />

l l<br />

l l<br />

l<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEMA 04/<br />

COB04MAR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL tt OF PANNINGS l ——————-————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CftLC V.G.<br />

SAMPLE tt PANNED ^^^^ rrsrsrsas cz^rrrr ErrSS flAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE GOLD<br />

-12 N 100 X 100 20 C l l<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

20-15 N NO VISIBLE GOLD<br />

l 16.7 90


l l l<br />

l<br />

l<br />

l l<br />

l<br />

l<br />

l l<br />

l l l<br />

l<br />

l<br />

l l<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB01APR.WRI<br />

TOTAL ft OF<br />

SAMPLE It<br />

PAWED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

21-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

. -04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10<br />

-11 N<br />

-12<br />

-13 N<br />

25 X 50<br />

50 X 50<br />

50 X 75<br />

75 X 150<br />

175 X 225<br />

300 X 300<br />

25 X 25<br />

50 X 50<br />

50 X 75<br />

75 X 75<br />

75 X 175<br />

-14 N NO VISIBLE GOLD<br />

-15 25 X 75<br />

75 X 150<br />

125 X 175<br />

7'7'S V Vui<br />

BC<br />

10 C<br />

13 C<br />

22 C<br />

38 C<br />

54 C 1<br />

5 C<br />

10 C<br />

13 C<br />

15 C<br />

25 C 1<br />

10 C J<br />

22 C l<br />

2? C l<br />

to r i<br />

NUMBER OF GRAINS<br />

COGEMA 04,<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

rcsrrrrr srrssssrr r::;:::::: rsrrr HAG ASSAY<br />

T CMS PPB REMARKS<br />

6 21.3<br />

l<br />

4 12.6<br />

l<br />

669<br />

96<br />

1 18.0 161<br />

EST. 3X PYRITE<br />

EST. Ti. PYRITE<br />

ESI. IX PYRITE


1 111111111111111111<br />

PAGE 2<br />

COGEMA<br />

04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB01APR.WRI<br />

TOTA! ft flP PAMNIMfK 4 ————<br />

i u i nL. n u* rniiiiiiiuj <br />

ABRADED<br />

PAurM<br />

SAMPLE<br />

r<br />

(t<br />

u nAiinr*n<br />

PANNED srzzrss: : srsssssss ssrsrsrr rsrrs MAR AWAY<br />

BOB-87<br />

Y/N DIAMETER THICKNESS T<br />

-16 N NO VISIBLE GOLD<br />

-17 N NO VISIBLE GOLD<br />

NUMBER OF GRAINS<br />

IRREGULAR DELICATE TOTAL NON<br />

CALC V.G.<br />

P T P T P 6MS PPB<br />

4 19.4 1659<br />

22-01 N 75 X 100 IB C 1<br />

1<br />

1 17.6 57<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

23-01 N 100 X 100 20 C 1<br />

1<br />

1 17.1 88<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N 150 X 250 38 C 1<br />

1<br />

1 16.0 713<br />

-05 N 250 X 400 58 C 1<br />

1<br />

1 14.6 3088<br />

-06 N NO VISIBLE GOLD<br />

-07 N 50 X 75 13 C 1<br />

1<br />

1 14.5 26<br />

-08 N NO VISIBLE GOLD<br />

-09 N 125 X 200 31 C 1<br />

1<br />

1 15.6 400<br />

-t A N uri vTRirtiF Km n


l l l<br />

l l<br />

l l l<br />

l l<br />

l l l<br />

l l l l l<br />

l<br />

PAGE 3 COGEHA 04A<br />

BOLD CLASSIFICATION<br />

VISIBLE BOLD FROH SHAKING TABLE AND PANNING<br />

COB01AFR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL l OF RANKINGS 4 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE Hi PANNED srrrrrrr ^z^~ es^rssr rsrsr MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GHS PPB REMARKS<br />

BOB-87<br />

-11 N 150 X 225 36 C l l<br />

l 13.l 722<br />

-12 Y 25 X 50 8 C l l EST. 0.5X PYRITE<br />

200 X 325 48 C l l<br />

325 X 400 63 C l l<br />

24-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

24-07 N 50 X 125 IB C l l<br />

3 16.3 5343<br />

i il? w


1<br />

111111111111111111<br />

PAGE 1<br />

COGEMA<br />

04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TAELE AND PANNING<br />

cobo2apr. wrl<br />

DAMMIHrO<br />

TOTAL ft 0F rnNNlNbb 1<br />

NUMBER OF GRAINS<br />

"——— '——— .-.-— -.—— —*—— MMHHMKH...<br />

——.......<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

p- Au Til F" il<br />

SAMPLE It<br />

PANKFR<br />

r niftiwi/ B"—<br />

srzsrss::<br />

~— — ^— ^i.*...—<br />

ssrrsrrrs<br />

—— HWHW-~rrszsssr<br />

~—~***~<br />

——z<br />

|<br />

MAR<br />

\ftij riww*i<br />

ClWAV<br />

i<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

24-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

-17<br />

N 125 X 125 25 C 1 1<br />

1 18.6 156<br />

25-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

-08<br />

N 100 X 200 29 C 1 1<br />

1 12.8 386<br />

-09<br />

Y 25 X 25 5 C 1 1 EST. IX PYRITE<br />

75 X 75 15 C 1 1<br />

100 X 150 25 C 11<br />

3 11.0 323


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE 2 COGEHA MA<br />

t<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2apr.wri<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNIN6S i ——————————————-—————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE # PANNED ssrrsrrr zr-zzrrr rrrrrrzr:: ESSSE HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-li N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

-15 N NO VISIBLE GOLD<br />

-16 N NO VISIBLE GOLD<br />

-17 N NO VISIBLE GOLD<br />

-16 N 200 X 250 42 C l l<br />

26-01 N 200 X 200 38 C l l<br />

-02 N 100 X 200 29 C l l<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-i l N NO VISIBLE GOLD<br />

l 15.8 95<br />

l 12.2 1313<br />

l 17.0 671<br />

l 14.8 334


l l<br />

l l l<br />

l<br />

l l<br />

l l l<br />

l l l l<br />

l l<br />

l l<br />

PAGE 3 C06EMA 04/'<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2apr.wri<br />

NUMBER OF GRAINS<br />

TOTAL K OF PANNIN6S l -—————————————————-<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE 8 PANNED rrrrrsrr *:^^: srrzr^z Errzs MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

BOB-87<br />

26-12 N NO VISIBLE GOLD


PAGE 1<br />

COGEMA<br />

04/<br />

1 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

GOLD CLASSIFICATION<br />

E-rrrszsr;.. ———————<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB03flPR.li IR1<br />

NUMBER OF GRAINS<br />

OAMMTHrC A —~ ._ ~. _ ....—I_ H..H ._ ~.—....~..— ~<br />

TOTAL t Of rHnNlNbb 4 —————————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NOW CALC V.G.<br />

PAKINPH cr-sssss ss-ssssss sszrssrs ssrss MAR AWAY<br />

CAMP! F ft<br />

Onl liwC, tt<br />

BOB-87<br />

26-13<br />

-14<br />

-15<br />

-16<br />

-17<br />

-18<br />

-19<br />

-20<br />

-21<br />

-22<br />

-23<br />

27-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

W DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

N 200 X 250 42 C 1 1<br />

N<br />

NO VISIBLE GOLD<br />

N lOCi X 125 22 C 1 1<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

1 21.9 731<br />

1 18.5 115<br />

Y 25 X 25 5 C 1 EST. 3Z PYRITE<br />

75 X 100 IB C 1<br />

100 X 100 20 C 1<br />

100 X 125 22 C 1<br />

200 X 300 46 C 1<br />

5 20.5 1285<br />

Y 50 X 50 10 C 1 1 EST. 77. PYRITE<br />

50 X 75 13 C 1 1<br />

200 X 200 38 C 1 1


PAGE 2<br />

CQGEMA<br />

04/<br />

1 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB03APR.WRI<br />

NUMBER OF GRAINS<br />

ITUGC A ~. ..~ ___ _—.__ ~— -._ TOTAL 1 OF fmli HOO t —— ———— ~~ -— -——— ——-<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

3AMP1 F Ut PflHMFF) —— sss-s c ——— srs c-s ——— r ——— MAR AQQAV<br />

4<br />

BOB-B7<br />

-07 N<br />

-08 N<br />

-09 N<br />

-10 N<br />

-11 N<br />

-12 N<br />

-13 N<br />

-14 N<br />

26-01 N<br />

-02 N<br />

-03 N<br />

-04 N<br />

-05 Y<br />

-06 N<br />

-07 N<br />

29-01 N<br />

-02 N<br />

-03 H<br />

-04 W<br />

m DIAMETER THICKNESS T P T P T P QMS PPB REMARKS<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

100 X 150 25 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

75 X 100 18 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

1 14.4 201<br />

1 15.0 67<br />

50 X 50 10 C 1 1 EST. l'/. PYRITE<br />

150 X 150 29 C 1 1<br />

250 X 400 58 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

m wsmE GOLD<br />

3 11.1 4579


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE 3 ' COGEHA 04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

CQB03APR.HR1<br />

NUMBER OF GRAINS<br />

TOTAL tt OF PANNINGS 4 ————————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE f PANNED *:^^ -——-——-—— ssrrrrrs rrrrz HAG ASSAY<br />

y/N DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

BOB-87<br />

-05 N NO VISIBLE GOLD<br />

-06 Y 75 X 100 18 C l l EST. 3X PYRITE<br />

100 X 125 22 C l l<br />

-07 N NO VISIBLE GOLD<br />

29-08 N NO VISIBLE GOLD<br />

2 25.2 124


l l l l<br />

l<br />

l<br />

l l<br />

l l l<br />

l<br />

l l<br />

l l l l<br />

l<br />

PAGE l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04APR.WRI<br />

TOTAL # OF PANNINGS 3 ——<br />

ABRADED<br />

SAMPLE l PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

29-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

N<br />

N<br />

N<br />

N<br />

N<br />

-14 N<br />

-15<br />

30-01<br />

-02<br />

-03<br />

N<br />

-04 V<br />

-05 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

50 X 75<br />

300 X 400<br />

NO VISIBLE GOLD<br />

N 500 X 550 83 C<br />

D VISIBLE GOLD<br />

50 X 50<br />

75 X 100<br />

75 X 200<br />

100 X 125<br />

25 X 25<br />

50 X 50<br />

50 X 100<br />

75 X 10(i<br />

125 X 225<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-fiQ M tin l HOT DI C om n<br />

13 C l<br />

61 C l<br />

10 C<br />

IB C<br />

27 C<br />

22 C<br />

5 C<br />

10 C<br />

15 C<br />

16 C<br />

34 C l<br />

NUMBER OF GRAINS<br />

COGEMA 04,<br />

IRREGULAR DELICATE TOTAL NON<br />

P T P T P GMS<br />

l<br />

l 14.9<br />

l<br />

2<br />

l<br />

l<br />

1<br />

l 22TT<br />

l<br />

2<br />

13.4<br />

l 14.9<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

25<br />

l 15.6 3607<br />

l 15.4 11099<br />

326<br />

215<br />

519<br />

EST. 3'/. PYRITE<br />

EST. IX PYRITE


PAGE 2 COGEHA M/<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

COB04APR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL i OF PANNINGS 3 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE'* PANNED ssss-sr srrrr^r rrrrrrsr srrrr MAG ASSAY<br />

V/H DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-87<br />

-09 N NO VISIBLE GOLD<br />

-10 N 225 X 275 46 C l l<br />

-li N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

-15 N NO VISIBLE GOLD<br />

-16 N NO VISIBLE GOLD<br />

-17 N NO VISIBLE GOLD<br />

-18 N NO VISIBLE GOLD<br />

-19 N NO VISIBLE GOLD<br />

l 14.4 1506<br />

-20 Y NO VISIBLE GOLD EST. 50X PYRITE<br />

31-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N 250 X 500 65 C i l


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE 3 COGEMA 04/<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04APR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNIN6S 3 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE f PANNED rrrrrrrr ———^. rssrrrzr rrzrr MA6 ASSAY<br />

m DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-11 N NO VISIBLE GOLD<br />

-12 . N NO VISIBLE GOLD<br />

31-13 N NO VISIBLE GOLD<br />

l 16.6 4110


1 11111<br />

1 111111111111<br />

PAGE 1<br />

COGEMA<br />

04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB05APR. HR1<br />

NUMBER OF GRAINS<br />

TOTAL S 0F PANNINGS 4 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

CflMpI Oru II LU C ft li PANNED ssssssss s..sssssa rssssssB srsrr HftQ ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-87<br />

31-14<br />

N 125 X 175 29 C 1 1<br />

1 17.8 277<br />

-15<br />

Y 75 X 75 15 C 1 1 EST. 57. PYRITE<br />

75 X 125 20 C 2 2<br />

150 X 225 36 C 1 1<br />

4 15.9 624<br />

-16<br />

-17<br />

-18<br />

N 175 X 225 36 C 1 1<br />

N<br />

NO VISIBLE GOLD<br />

1 15.6 731<br />

Y 25 X 25 5 C 1 1 EST. 17. PYRITE<br />

50 X 100 15 C 1 1<br />

200 X 325 48 C 1 1<br />

3 17.9 1430<br />

-19<br />

-20<br />

-21<br />

-22<br />

-23<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

32-01<br />

N 175 X 375 50 C 1 1<br />

-02<br />

-03<br />

-04<br />

-05<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

1 22.1 1288<br />

-06<br />

N 100 X 225 31 C 1 1<br />

1 17 t ViP


1 111111111111111111<br />

PAGE 2<br />

COGEMA<br />

04/<br />

GOLD CLASSIFICATION<br />

rrsrssrrrzr—rrz ———<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB05APR.WRI<br />

TOTAL it OF PANN INbS 4<br />

CAMP'1 Onl irLL, F ir it<br />

BOB-87<br />

rnliru. PANKIF<br />

Y/N<br />

NUMBER OF GRAINS<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

D srssrsss ss^s^ss rrsrsssr ssass HAG ASSAY<br />

DIAMETER THICKNESS T P T P T P GM3 PPB REMARKS<br />

-07 N<br />

-06 N<br />

-09 Y<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

50 X 50 10 C 11 EST. 107. PYRITE<br />

75 X 175 25 C 1 1<br />

125 X 175 29 C 1 1<br />

3 15.5 517<br />

-10 N<br />

-11 N<br />

-12 N<br />

-13 N<br />

33-01 N<br />

-02 N<br />

-03 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

75 X 125 20 C 1 1<br />

1 14.4 104<br />

-04 Y<br />

25 X 25 5 C 1 EST. IX PYRITE<br />

5* X 150 20 C 1<br />

150 X 350 46 C 1<br />

350 X 350 61 C 1<br />

500 X 700 90 C 1<br />

5 21.6 14930<br />

-05 N<br />

75 X 200 27 C 1 1<br />

1 21.1 181<br />

-06 N<br />

-07 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

-OB<br />

N<br />

NO VISIBLE GOLD<br />

-0? N<br />

m VISIBLE GOLD


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l llllllllllll<br />

t<br />

PAGE 3 COGEHA 04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB05AFR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL tt OF PANNINSS 4 ————————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NUN CALC V.G.<br />

SAMPLE S PAWED z^^ ------^- SBit8888. SS5SS MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-10 N NO VISIBLE GOLD<br />

-li N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

34-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

34-03 N NO VISIBLE GOLD


1 111111111111111111<br />

PAGE 1<br />

C06EMA<br />

04;<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PAWING<br />

COB06APR.WRI<br />

TOTAL ft OF PANNI<br />

^WlPI dnitTLu F 8 tt<br />

PAMUPn<br />

rniuiuL.'<br />

Y/N<br />

NUMBER OF GRAINS<br />

4<br />

——— ———-~—— -————--- --<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

j. —----- ------j.— C!srs-S!r. ----- MAR fiQQAY<br />

DIAMETER THICKNESS T P T P T P GM3 PPB REMARKS<br />

BOB-87<br />

34-04 N<br />

-05 N<br />

-06 N<br />

-07 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

m VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

-OB<br />

N<br />

NO VISIBLE GOLD<br />

-09 N<br />

-10 N<br />

-11 N<br />

-12 N<br />

-13 Y<br />

-14 N<br />

-15 N<br />

-16 N<br />

-17 N<br />

35-01 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

100 X 225 31 C 1 1 EST. 3X PYRITE<br />

15V. MARCASITE PELLETS<br />

1 22.2 231<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

100 X 200 29 C 1 1<br />

S 13.3 371<br />

-02 N<br />

-03 N<br />

NO VISIBLE SOLD<br />

100 X 125 22 C 1 1<br />

*<br />

-04 Y<br />

1 26.9 79<br />

50 X 50 10 C 1 1 EST. 3X PYRITE<br />

75 X 175 25 C 1 1 75 MARCASITE PELLETS<br />

175 X 225 36 C i 1<br />

3 16.9 7o6


l l l l<br />

l l<br />

l l l l l<br />

l l l<br />

l<br />

l l<br />

l l<br />

PAGE 2 CGGEHA 04/<br />

GOLD CLASSIFICATION<br />

rrzrrsrzrrsrzsrzsrs<br />

VISIBLE GOLD FROM SHAKINS TABLE AND PANNING<br />

COB06APR.WRI<br />

tun*, ff ur rrirtiiNoa<br />

QiMPI C f POMMPn<br />

GrinrLt fi rnnii\CU<br />

Y/N<br />

BOB-87<br />

DIAMETER<br />

50 X<br />

50 X<br />

100 X<br />

200 X<br />

t<br />

75<br />

100<br />

125<br />

225<br />

-06 N NO VISIBLE GOLD<br />

NUMBER OF GRAINS<br />

ABRADED IRREGULAR DELICATE TOTAL KON CALC V.G.<br />

rs — sr — z. — sz~~ sssrsrzs rzszs (WR A33AV<br />

THICKNESS T P T P T P GMS PPB REMARKS<br />

13 C 11<br />

15 C 1 1<br />

22 C 1 1<br />

40 C 1 l<br />

-07 N 75 X 100 18 C l l<br />

-08 N 75 X 150 22 C l l<br />

-09<br />

36-01<br />

-02<br />

•--03<br />

-04<br />

-05<br />

N<br />

N<br />

N<br />

N<br />

Y<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

2-5 X 25 5 C 1<br />

75 X 75 15 C 1<br />

75 X 125 20 C 1<br />

100 X 125 22 C 1<br />

150 X 150 29 C 1<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-M H HI) yTQriy r mi n<br />

6 13.5 1242<br />

l 6.2 163<br />

1<br />

1<br />

1<br />

1<br />

345<br />

4 14.5 296<br />

1<br />

3 16.0 308<br />

EST. 3X PYRITE


l l l l l<br />

l<br />

l l l<br />

l l l l l<br />

l l l l<br />

l<br />

PAGE 3 COGEHA 04/<br />

t<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB06fiPfi.WRI<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNIN5S 4 —.———-—————.—.<br />

ABRADED IRRE6U.AR DELICATE TOTAL NDN CALC V.G.<br />

SAMPLE * PANNED ======~ rrrsrrrrr ^^^ rssr.- MA6 ASSAY<br />

Y/N DIAMETER THICKNESS T F T P T P GHS PPB REMARKS<br />

BOB-8?<br />

-12 N 75 X 75 15 C i S<br />

-13 N 75 X 100 18 C l l<br />

-14 N NO VISIBLE GOLD<br />

-15 N NO VISIBLE GOLD<br />

37-01 N 100 X 150 25 C l l<br />

37-02 N NO VISIBLE GOLD<br />

l 17.0 38<br />

l 13.3 76<br />

l 19.2 151


l l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

PAGE l COGEMA 04/<br />

BOLD CLASSIFICATION<br />

VISIBLE BOLD FROM SHAKING TABLE AND PANNING<br />

cobo7apr.wri<br />

NUMBER OF BRAINS<br />

TOTAL i OF PANNINGS l ——————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAHPLE l PANNED *^~ ^^r*** ^-^--..-- w^ HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-97<br />

37-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE BOLD<br />

-07 N 325 X 425 65 C l l<br />

-08 N NO VISIBLE BOLD<br />

-09 N 300 X 300 54 C l I<br />

-10 N 100 X 150 25 C l l<br />

-li N 125 X 125 25 C l l<br />

-12 N 100 X 175 27 C l l<br />

-13 N NO VISIBLE GOLD<br />

-14 N 75 X 100 IB C l l<br />

-15 N NO VISIBLE GOLD<br />

-16 N NO VISIBLE GOLD<br />

-17 N NO VISIBLE BOLD<br />

-18 N NO VISIBLE GOLD<br />

-19 N NO VISIBLE BOLD<br />

i 19.2 3553<br />

l 16.7 2163<br />

l 32.2 90<br />

l 21.6 134<br />

l 24.6 156<br />

l 16.3 62<br />

-~x\ y TO y too is r 1 i FRT. iv. PVRITF


1 1<br />

C 2 COGEMA<br />

04,<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo7apr.wri<br />

NUMBER OF GRAINS<br />

TOTAL 1 OF PANNINGS 1 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE t PANNED arscsssr cscsccrcn rr^^ ^s* MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

BOB-97<br />

-21<br />

-22<br />

-23<br />

38-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

75 X 100 18 C 1 1<br />

125 X 175 29 C 1 1<br />

300 X 400 61 C 1 1<br />

NO VISIBLE GOLD<br />

400 X 500 74 C 1 1<br />

100 X 150 25 C 1 i<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

' NO VISIBLE GOLD<br />

NO VISIBLE BOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

AW VISIBLE GOLD<br />

3 24.3 271<br />

1 15.5 3631<br />

1 14.6 7724<br />

1 16.2 159<br />

1 l '


l l l<br />

l l<br />

l<br />

l l l l<br />

l l l<br />

l l<br />

l l l<br />

l<br />

PAGE 3 COGEMA 04,<br />

)<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo7apr.wri<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNIN6S l —————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G,<br />

SAMPLE t PANNED **^~ rr^rrsrr .r^nts ^s HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-97<br />

-16 N NO VISIBLE GOLD<br />

39-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

39-03 N 100 X 150 25 C l l<br />

l<br />

20^2143


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

l l<br />

l<br />

4T<br />

l COGEMA M/<br />

GOLD aASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB08APR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNINGS 2 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NOW CALC V.G.<br />

SAMFtE l PANNED sssrrss: ^---^------ ^--^ rrrsr HAG ASSAY<br />

Y/N DIAMETER THICKNESS TPTPTP GMS PPB REMARKS<br />

BOB-87<br />

39-04 N NO VISIBLE GOLD<br />

-05 N 75 X 75 15 C l l<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE GOLD<br />

-12 N 100 X 175 27 C l l<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

-15 N NO VISIBLE GOLD<br />

-16 N 75 X 125 20 C l l<br />

-17 N NO VISIBLE GOLD<br />

41-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

42-01 N NO VISIBLE GOLD<br />

l 17.5 37<br />

l 17.4 220<br />

l 15.9 94<br />

km iiTr*Tf-ii r-


l l<br />

l l l<br />

l<br />

l l l<br />

l l<br />

l l l<br />

l l l l<br />

l<br />

PAGE 2<br />

GOLD CLASSIFICATION<br />

VISIBLE BOLD FROM SHAKING TABLE AND PANNING<br />

C06EMA 04/<br />

COB08APR.WR1<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNIN6S 2 ——<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V,6.<br />

SAMPLE S PANNED<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 Y 100 X 125 22 C<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

43-01 N NO.VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 Y NO VISIBLE GOLD<br />

45-01 N NO VISIBLE GOLD<br />

46-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

47-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

47-03 N NO VISIBLE GOLD<br />

2 21.1 201<br />

EST. 3Z PYRITE<br />

EST, 3X PYRITE<br />

3X MARCASITE PELLETS


l l<br />

l l<br />

l l<br />

l<br />

l l<br />

l l<br />

l<br />

l l<br />

l l<br />

l l<br />

l<br />

PAGE l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEMA 04,<br />

cobo9apr.wri<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNIN6S B ——<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE tt PANNED<br />

s:;::::: assent rrrssrrr rrrrs HAG ASSAY<br />

Y/N DIAMETER THICKNESS<br />

6MS PPB REMARKS<br />

BOB-87<br />

47-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 25 X 50<br />

49-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

51-01 N HO VISIBLE GOLD<br />

-02 Y NO VISIBLE GOLD<br />

52-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

53-01 N NO VISIBLE GOLD<br />

54-01 N NO VISIBLE GOLD<br />

-02 N 125 X 150<br />

-03 N 150 X 250<br />

55-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N 150 X 175<br />

-m H an UTCTPI c mi n<br />

8 C<br />

27 C l<br />

38 C l<br />

31 C l<br />

l 18.4<br />

l<br />

l 29.9<br />

l<br />

l 21.6<br />

l 20.6<br />

128<br />

528<br />

303<br />

EST. 10X PYRITE<br />

EST. 10X PYRITE


1 111111111111111111<br />

PAGE 2<br />

COGEMA<br />

04/:<br />

GOLD CLASSIFICATION<br />

rsrrsrrrzsrrrrrsrrs<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo9apr.Hrl<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNINGS 6 ————<br />

ABRADED IRREGULAR DELICATE TOTAL WON<br />

^flMPI 3ni ir ut F tt it PANNFR rnriiiti/ sszssrss ——— .-—.—-<br />

Y/N DIAMETER THICKNESS T P T P T P CMS<br />

CALC V.G.<br />

fiCCflV nwwni<br />

PPB REMARKS<br />

BOB-87<br />

-06 Y 50 X 75 13 C 2<br />

75 X 125 20 C<br />

150 X 200 34 C 1<br />

300 X 350 58 C 1<br />

1 1<br />

11<br />

5 21.1<br />

2<br />

EST. 2X PYRITE<br />

2639<br />

-07 Y 100 X 125 22 C 1<br />

1<br />

EST. IX PYRITE<br />

1 18.6<br />

113<br />

56-01 N NO VISIBLE GOLD<br />

-02 Y 100 X 150 25 C 1<br />

175 X 200 36 C 1<br />

1<br />

1<br />

EST. l 1/;<br />

PYRITE<br />

2 21.8<br />

566<br />

-03 Y 125 X 150 27 C 1<br />

175 X 200 36 C<br />

200 X 275 44 C 1<br />

250 X 275 48 C 1<br />

400 X 675 84 C 1<br />

1<br />

1 1<br />

1<br />

1<br />

1<br />

EST. 0.5X PYRITE<br />

5 25.3<br />

9443<br />

57-01 N NO VISIBLE GOLD<br />

-02 N 100 X 125 22 C 1<br />

1<br />

1 16.6<br />

126<br />

58-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

59-01 N 250 X 300 50 C 1<br />

1<br />

1 16.1<br />

1573<br />

-02 N 100 X 125 22 C 1<br />

1<br />

1 20 6<br />

103


l l l l l<br />

l l l l<br />

l l l<br />

l l l<br />

l<br />

l l l<br />

PAGE 3<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo9apr.Hrl<br />

TOTAL t OF PANNINGS 8 ——<br />

ABRADED<br />

SAMPLE l PANNED<br />

Y/N DIAMETER THICKNESS T<br />

BOB-87<br />

-03<br />

-04<br />

-05<br />

60-01<br />

-02<br />

-03<br />

-04<br />

61-01<br />

61-02<br />

N<br />

NO VISIBLE GOLD<br />

N 100 X 200 29 C<br />

N<br />

N<br />

Y<br />

N<br />

Y<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

100 X 150<br />

150 X 150<br />

NO VISIBLE GOLD<br />

50 X 50<br />

100 X 250<br />

200 X 300<br />

225 X 600<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

25 C 1<br />

29 C 1<br />

10 C<br />

34 C 1<br />

46 C 1<br />

70 C<br />

NUMBER OF BRAINS<br />

COGEhA 04/:<br />

IRREGULAR DELICATE TOTAL NON<br />

^^^ r^rrrrsz ~~^z srrss flftG<br />

T T CMS<br />

1 25.9<br />

2 18.8<br />

4 19.5<br />

CALC V.G.<br />

PPB<br />

191<br />

416<br />

6074<br />

REMARKS<br />

EST. 3X PYRITE<br />

EST. IX PYRITE


1 111111111111111111<br />

PAGE 1<br />

COGEMA<br />

04,<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COBOAAPR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL # OF PANNINGS 8 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL<br />

CfiMffl C a PANWFn rsrrsssr ssrsrrsss sr — zcrs srsss<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

m CALC V.G.<br />

MAC AWAY<br />

1 KiU flwwrl I<br />

6MS PPB REMARKS<br />

BOB-87<br />

61-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-OB N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-11 Y 50 X 75 13 C 1 1<br />

75 X 100 18 C 1 1<br />

125 X 175 29 C 1 1<br />

EST, 17. PYRITE<br />

3<br />

15.9 397<br />

-12 N 125 X 150 27 C 1 1<br />

1<br />

26.5 144<br />

-13 Y 150 X 200 34 C 1 1<br />

175 X 300 44 C 1 1<br />

175 X 600 66 C 1 1<br />

300 X 425 63 C 1 1<br />

EST. IX PYRITE<br />

1 GRAIN GALENA<br />

4<br />

28.6 5708<br />

62-01 Y 25 X 50 B C 1 1<br />

50 X 75 13 C 1 1<br />

75 X 200 27 C 1 1<br />

EST, U PYRITE<br />

3<br />

15.1 284<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD


1 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

^<br />

9<br />

PAGE 2<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

C06EMA<br />

CQBOAAPR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL 1 OF PANNINGS 8 ——————————————-——<br />

SAMPLE 1<br />

PANNED<br />

V/N<br />

BOB-87<br />

-06 Y<br />

-07 N<br />

-08 N<br />

-09 N<br />

-10 N<br />

-11 N<br />

63-01 N<br />

64-01 N<br />

-02 N<br />

-03 N<br />

65-01 N<br />

-02 N<br />

-03 Y<br />

-04 Y<br />

66-01 N<br />

67-03 N<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

rsBSBBSs srssssszB cr—srsr rss flAG ASSAY<br />

DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

50 X 50 10 C 1 1 EST. 55X PYRITE<br />

100 X 125 22 C 1 t<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE 60LD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

450 X 550 80 C 1 1<br />

NO VISIBLE GOLD<br />

175 X 200 36 C 1 1<br />

NO VISIBLE GOLD<br />

2 26.3 88<br />

1 21.5 6977<br />

1 30.4 311<br />

75 X 100 18 C 1 1 EST. IX PYRITE<br />

75 X 125 20 C 1 1<br />

100 X 200 29 C 1 1<br />

300 X 300 54 C 1 1<br />

4 22.9 1917<br />

100 X 150 25 C 1 1 EST. 0.25X PYRI<br />

100 X 175 27 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

2 32.0 210<br />

04/


l l l l<br />

l l<br />

l l<br />

l l l l l l l<br />

l l<br />

l l<br />

PAGE 3<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEHA<br />

COBOAAPR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL l OF FflNNINGS 8 ——<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE t PANNED<br />

rrrrrrrr rrrr:::::: srssrrrz SSSSS MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

B-87<br />

-02 N<br />

-03 N<br />

-05 Y<br />

-06 N<br />

-07 N<br />

VISIBLE GOLD<br />

VISIBLE GOLD<br />

50 X 75<br />

75 X 75<br />

75 X 100<br />

100 X 200<br />

150 X 200<br />

VISIBLE GOLD<br />

13 C 1<br />

15 C<br />

18 C<br />

29 C<br />

34C 1<br />

50 X 100 15 C l<br />

70-01 N 100 X 300 38 C l<br />

-02 Y 25 X 100 13 C<br />

72-01 N 50 X 75 13 C l<br />

1<br />

1<br />

1<br />

5 14.5 1014<br />

l<br />

l<br />

l<br />

14T<br />

l 30.3<br />

l<br />

l 100.2<br />

l<br />

l<br />

isTF<br />

46<br />

376<br />

25<br />

EST, 3Z PYRITE<br />

EST. 3X PYRITE<br />

04,


1 1<br />

4<br />

PAGE 1 COGEMA 04/<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COBOBAPR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL 1 OF PANNIN6S 6 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE t PANNED nssBBBBs ------ -----^ s-srr MftQ ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

72-02<br />

-03<br />

73-01<br />

74-01<br />

-02<br />

77-01<br />

-02<br />

78-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

79-01<br />

-02<br />

80-01<br />

Y 75 X 100 18 C 1 1 EST. IX PYRITE<br />

75 X 125 20 C 1 1<br />

N 75 X 125 20 C 1 1<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

N 150 X 225 36 C 1 1<br />

N 75 X 100 18 C 1 1<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

N 150 X 200 34 C 1 1<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

2 15.3 164<br />

1 12.2 123<br />

1 16.1 587<br />

1 20.2 50<br />

1 24.9 311<br />

Y 100 X 100 20 C 1 1 EST. 17. PYRITE<br />

150 X 300 42 C 1 1<br />

N 150 X 150 29 C 1 1<br />

N<br />

NO VISIBLE GOLD<br />

2 23.6 742<br />

1 32.6 151<br />

Y 25 X 25 5 C 1 1 EST. 20Z PYRITE<br />

50 K 50 10 C l l<br />

75 V 1ftft ifi r 1 l


C06EMA 04;<br />

l ll<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

GOLD CLASSIFICATION<br />

rrrrrrrrz:rrrrrrrr:<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

i<br />

COBOBAPR.WRI<br />

NUMBER OF GRAINS<br />

HL * W rHNHUNUD 0 —————————————————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

RE i PANNED ssssssss ^^;^ r^^r SESSS MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB<br />

JOB-87<br />

82-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

83-01<br />

84-01<br />

-02<br />

-03<br />

-04<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

Y<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

75 X 75 15 C 1 1<br />

125 X 150 27 C 1 1<br />

150 X 250 38 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

50 X 150 20 C 1 1<br />

NO VISIBLE GOLD<br />

150 X 150 29 C 1 1<br />

-05 N ISO K 200 34 C t l<br />

3 37.1 33<br />

3 21.3 745<br />

1 17.9 84<br />

l 25.1 197<br />

EST. IX PYRITE


l l<br />

l l l l<br />

l l l l l<br />

l l l l l l<br />

l l<br />

PAGE 3 COGEMA 04/<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COBOBAPR.WRI<br />

NUMBER OF GRAINS<br />

TOTAL i OF PANNINGS 6<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAHFLE i PANNED<br />

rrsrrsrs r^^z ssssssss CSSES ^Q ASSAY<br />

Y/N DIAMETER THICKNESS<br />

T<br />

T<br />

GMS PPB REMARKS<br />

BOB-87<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

85-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 Y 150 X 200<br />

-04 N<br />

85-05<br />

50 X 100<br />

50 X 75<br />

75 X 100<br />

100 X ISO<br />

34 C l<br />

15 C l<br />

13 C<br />

18 C<br />

25 C<br />

i 28.7<br />

1<br />

1 21.2<br />

1<br />

1 17.3<br />

1<br />

2<br />

1<br />

270<br />

365<br />

37<br />

4 15.6 339<br />

EST. 3X PYRITE


1 111111111111111111<br />

PAGE<br />

i<br />

COGEMA<br />

05,<br />

GOLD CLASSIFICATION .<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COBOCAPR.WRI<br />

NUMBER OF BRAINS<br />

TOTAL t OF PANNINGS<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

—— -————— ~. . -- -.— .— .—— .— .—- MAP AOPAU<br />

SAMPLE S PANNED — ~— ————— ——— ~ —— mu nMm<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

85-06 N NO VISIBLE GOLD<br />

-07 N 150 X<br />

200 34 C i 1<br />

I 22.8 339<br />

-08 N 150 X<br />

175 31 C 1 1<br />

1 22.6 276<br />

-09 N NO VISIBLE GOLD<br />

86-01 N 150 X 200 34 C 1 1<br />

1 17.0 455<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N 150 X<br />

175 31 C 1 1<br />

1 18.0 346<br />

-05 V 25 X<br />

125 X<br />

200 X<br />

250 X<br />

25 5 C 1 1 EST. 37. PYRITE<br />

175 29 C 1 1<br />

250 42 C 1 1<br />

275 48 C 1 1<br />

4 16.7 2749<br />

87-01 N NO VISIBLE GOLD<br />

-02 N 150 X<br />

200 34 C 1 1<br />

1 21.0 368<br />

-03 N 150 X<br />

400 50 C 1 1<br />

1 16.5 1725<br />

88-01 Y 50 X<br />

75 X<br />

150 X<br />

100<br />

75<br />

15 C<br />

15 C<br />

2<br />

1<br />

2<br />

1<br />

EST. 3X PYRITE<br />

225 36 C 1 1


1 111111111111111111<br />

JAGE2<br />

COGEHA<br />

05/<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COBOCAPR.WRI<br />

TflTAI<br />

i u i ML.<br />

ft<br />

ir<br />

flF<br />

ur<br />

PANNING<br />

r fii\n i iiUvi<br />

7<br />

i<br />

————— -<br />

ABRADED<br />

Y/N DIAMETER THICKNESS T<br />

NUMBER OF GRAINS<br />

IRREGULAR DELICATE TOTAL<br />

P T P T P<br />

NON CALC V,G.<br />

MAR WMY<br />

rinw njwni<br />

6MS PPB REMARKS<br />

BOB-87<br />

-02 Y 50 X 75 13 C 2<br />

100 X 150 25 C<br />

2<br />

1 1<br />

EST, 5X PYRITE<br />

3<br />

16.1 226<br />

-03 Y 50 X 75 13 C 1<br />

75 X 125 20 C<br />

75 X 150 22 C 1<br />

100 X 150 25 C<br />

1<br />

1 1<br />

1<br />

1 1<br />

EST. 101/.<br />

PYRITE<br />

4<br />

17.4 396<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 Y NO VISIBLE GOLD<br />

EST. 207. PYRITE<br />

89-01 N NO VISIBLE GOLD<br />

-02 Y 50 X 75 13 C 1<br />

75 X 100 18 C 1<br />

1<br />

1<br />

EST. 7X PYRITE<br />

2<br />

21.3 65<br />

-03 N NO VISIBLE GOLD<br />

-04 Y 50 X 75 13 C<br />

100 X 150 25 C 1<br />

100 X 250 34 C 1<br />

1 1<br />

1<br />

1<br />

EST. 0.5X PYRITE<br />

3<br />

17.2 640<br />

-05 N 50 X 125 18 C 1<br />

1<br />

1<br />

21.3 47<br />

-06 N 75 X 100 18 C 1<br />

1<br />

1<br />

18.3 55<br />

-07 N 175 X 450 56 C<br />

1 1<br />

1<br />

24.1 1698<br />

-no ft f t-.ici i/rcrof c ecu n


l<br />

l i<br />

PAGE 3 COGEMA OS/i<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

l<br />

COBOCAPR.WRI<br />

NUMBER OF BRAINS<br />

TOTAL f OF PANNINGS 7<br />

ll<br />

l<br />

llllllllllll<br />

SAMPLE t<br />

PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

90-01 N NO VISIBLE GOLD<br />

ABRADED<br />

IRREGULAR<br />

T P T P<br />

DELICATE TOTAL NON<br />

CALC V.G.<br />

TP 6MS PPB<br />

-02 N 175 X 475 56 C<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N 50 X 50 10 C<br />

-06 N 50 X 75 13 C<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE GOLD<br />

90-12 N 100 X 150 25 C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1 19.6 2332<br />

1<br />

1 19.9 10<br />

1<br />

1 19.5 19<br />

1<br />

1 20.4 142


l l l<br />

l l l<br />

l l l l l l l l l l l l<br />

l<br />

PAGE l COGEMA OS/<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROh SHAKING TABLE AND PANNING<br />

cobodapr.wri<br />

NUMBER OF GRAINS<br />

TOTAL ft OF PANNIN6S 3 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE S PANNED rzrsrrrr rrr^rrzz z^^^ CKSS MAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PP6 REMARKS<br />

BQB-e?<br />

90-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

91-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N 75 X 100 IB C l l<br />

-05 N NO VISIBLE GOLD<br />

-06 N 100 X 100 20 C i l<br />

-07 N NO VISIBLE GOLD<br />

92-01 N 75 X 100 18 C l l<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

93-01 N 150 X 200 34 C l l<br />

-02 N 200 l 400 54 C l l<br />

-03 N NO VISIBLE GOLD<br />

l 23.6 43<br />

l 26.6 56<br />

l 20.1 50<br />

l 15.9 487<br />

l 20.3 1796<br />

-04 Y 50 X 50<br />

10 C 1 l 1l 2<br />

EST. IX PYRITE<br />

75 X 75<br />

75 X 100<br />

100 X 150<br />

125 X 200<br />

J 75 X 20o<br />

15 C 1<br />

18 C 1<br />

25 C 1<br />

31 C 1<br />

34 C J<br />

1<br />

1<br />

1<br />

1<br />

1


l l l l l<br />

l<br />

l l l<br />

l l l l l<br />

l l<br />

l l<br />

l<br />

PAGE 2<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TAELE AND PANNING<br />

COGEMA<br />

cobodapr.wri<br />

NUMBER OF 6RAINS<br />

TOTAL # OF PANNINGS 3 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL WON CALC V.G.<br />

SAMPLE ft PANNED srrrrrrr rrrrrrzss ::r;Srzu srrrr HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS<br />

BOB-67<br />

-05 N 125 K 175 29 C l<br />

-06 Y 50 X 75<br />

150 X 150<br />

200 X 275<br />

94-01 N NO VISIBLE GOLD<br />

13 C l<br />

29 C l<br />

44 C l<br />

-02 N 250 X 350 54 C l<br />

-03 N 100 X 100 20 C l<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 Y 75 X 100<br />

75 X 125<br />

100 X 225<br />

95-01 N NO VISIBLE GOLD<br />

18 C<br />

20 C<br />

31 C<br />

-02 N 150 X 225 36 C l<br />

-03 N 100 X 150 25 C l<br />

-04 50 X 50 10 C l<br />

7 1B.3 1092<br />

l<br />

l 2M 187<br />

l<br />

l<br />

l<br />

3 21.8 U02<br />

i 18.9<br />

l<br />

l<br />

i<br />

l<br />

i<br />

i?T<br />

l 19.0<br />

UT<br />

1879<br />

79<br />

3 24.3 360<br />

490<br />

152<br />

11<br />

EST. IX PYRITE<br />

EST. 3V. PYRITE<br />

OS/


l l<br />

PAGE 3 COGEHA 05,<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PAWING<br />

l— cobodapr.wri NUMBER OF GRAINS<br />

l TOTAL t OF PANNINGS 3 —-———————-——-<br />

ABRADED IRREGULAR DELICATE TOTAL WON CALC V.G.<br />

SAMPLE i PANNED ^^^ ^^ : rrrzzrrr rzrzz (^ ASSAY<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

BOB-87<br />

Y/N DIAMETER THICKNESS T P T P T P GfiS PPB REMARKS<br />

95-05 N 45(i X 550 60 C i i<br />

l 19.B 7576


1<br />

1<br />

1 1111l1iiiiiiiiiiii<br />

Pftsei<br />

COGEMA<br />

07/24/8/<br />

60LD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB01JIL.WRI<br />

TOTAL 1 OF PANNINGS B ————<br />

ABRADED<br />

*?AMPI F li POMMPfi rs —— s:<br />

Y/N DIAMETER THICKNESS T<br />

NUMBER OF GRAINS<br />

IRREGULAR DELICATE TOTAL<br />

P T P T P<br />

NON<br />

CALC V.6.<br />

6MS PPB f<br />

BOB-87<br />

96-01 Y 50 X 50 10 C<br />

50 X 75 13 C 1<br />

75 X 125 20 C 1<br />

1 1<br />

1<br />

1<br />

fNO SULPHIDES<br />

3<br />

32.6 63<br />

-02 N 50 X 75 13 C 1<br />

1<br />

i<br />

25.3 15<br />

-03 N NO VISIBLE GOLD<br />

-04 N 50 X 50 10 C 1<br />

1<br />

1<br />

23.7 8<br />

-05 N 75 X 75 15 C 1<br />

1<br />

1<br />

19.3 33<br />

-06 N 50 X 50 10 C 1<br />

1<br />

1<br />

19.8 10<br />

-07 N 50 X 75 13 C 1<br />

1<br />

1<br />

17.0 22<br />

-08 N 100 X 175 27 C 1<br />

1<br />

1<br />

18.6 206<br />

-09 N NO VISIBLE GOLD<br />

-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE BOLD<br />

-12 Y 50 X 100 15 C 1<br />

175 X 200 36 C 1<br />

1<br />

1<br />

EST. 2Z PYRITE<br />

2<br />

23.0 439<br />

-13 Y 25 X 25 5 C<br />

50 X 50 10 C 1<br />

75 X 100 18 C<br />

100 X 125 22 C 1<br />

1 1<br />

1<br />

2 2<br />

1<br />

EST. IX PYRITE


PR6E2<br />

CDGEMA<br />

07/24/87<br />

1 11<br />

60LD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

COB01JUL.WRI<br />

TOTAL ft OF PANNINGS<br />

SAMF1E ft<br />

BOB-87<br />

-14<br />

-15<br />

-16<br />

97-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-H<br />

-12<br />

-13<br />

PANNED<br />

Y/N<br />

Y<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

Y<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

n<br />

NUMBER OF GRAINS<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

rsrrrcsr srrssrssr cscsssss sssss flftG ASSAY<br />

DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

5 23.5 186<br />

50 X 50 10 C 1 1 EST. 17. PYRITE<br />

50 X 100 15 C 1 1<br />

75 X 75 15 C 1 1<br />

75 X 100 IB C 1 1<br />

50 X 50 10 C 1 1<br />

4 18.6 134<br />

1 21.1 9<br />

50 X 75 13 C 1 1 NO SULPHIDES<br />

75 X 75 15 C 1 1<br />

200 X 200 38 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

175 X 225 38 C 1 . 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

3 23.2 535<br />

1 28. B 396


l l l l<br />

l<br />

l<br />

l<br />

l l l l<br />

l l<br />

l l<br />

l l<br />

l<br />

PAGE 3<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB01JUL.WRI<br />

TOTAL t OF PANNINGS<br />

SAMPLE t PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

-14<br />

-15<br />

8<br />

25 X 25<br />

25 X 50<br />

50 X 75<br />

75 X 100<br />

25 X 25<br />

50 X 50<br />

50 X 75<br />

98-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE- GOLD<br />

-06<br />

-07 N<br />

-08 N<br />

125 X 150<br />

125 X 275<br />

100 X 100<br />

25 X 50<br />

98-09 N NO VISIBLE GOLD<br />

5C<br />

8C<br />

13 C<br />

18 C<br />

5C<br />

10 C<br />

13 C<br />

27 C<br />

38 C<br />

ABRADED<br />

NUMBER OF GRAINS<br />

C06EMA 07/24/87<br />

IRREGULAR DELICATE TOTAL NON<br />

T P T P T P BUS<br />

2<br />

l<br />

20 C l<br />

8C<br />

l<br />

6 32.2<br />

1<br />

2<br />

l<br />

4 30.5<br />

2 28.5<br />

l<br />

l 26.0<br />

I<br />

l 14.2<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

89<br />

534<br />

58<br />

EST. U PYRITE<br />

EST. IX PYRITE<br />

EST. IX PYRITE


1 111111111111111111<br />

PME1<br />

COGEMA<br />

07/27/8<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2jul.wri<br />

TOTAL 1 OF PAKNIN6S 16 ———<br />

SAMPLE 1 PANNED<br />

ABRADED<br />

ssrsss-<br />

Y/N DIAMETER THICKNESS T<br />

NUMBER 'OF GRAINS<br />

IRREGULAR DELICATE TOTAL NON<br />

CALC V.G.<br />

m<br />

:<br />

BtVMMM B ——. HV.H UM*<br />

—— r — srs ssasss— — ass flftG<br />

AfWllf<br />

ASSAY<br />

P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

98-10 N 50 X 75 13 C 1<br />

1<br />

1 19.6 19<br />

-11 N 75 X 100 18 C 1<br />

1<br />

1 23.4 43<br />

-12 N NO VISIBLE GOLD<br />

99-01 N NO VISIBLE GOLD<br />

-02 N 100 X 125 22 C 1<br />

1<br />

1 14.2 149<br />

-03 N NO VISIBLE GOLD<br />

-MY 25 X 50 8 C<br />

50 X 75 13 C 1<br />

75 X 75 15 C 2<br />

75 X 100 18 C 1<br />

2 2 EST. IX PYRITE<br />

1<br />

2<br />

1<br />

6 25.2 112<br />

100-01 N 175 X 250 40 C 1<br />

1<br />

1 26.3 516<br />

-02 N 75 X 100 IB C 1<br />

^<br />

-03 N 50 X 75 13 C i'"<br />

1<br />

1 24.4 41<br />

1<br />

1 22.6 17<br />

-04 N NO VISIBLE GOLD<br />

-05 Y 50 X 50 10 C<br />

50 X 75 13 C 1<br />

50 X 100 15 C<br />

75 X 100 18 C 1<br />

2 2 EST. 2Z PYRITE<br />

1<br />

1 1<br />

1<br />

5 27.9 86<br />

-06 r 25 K 25 5 C<br />

i 1 EST. 27. PYRITE


1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1111111<br />

1<br />

PffiL2<br />

BOLD CLASSIFICATION<br />

srsrrrrrrszsszrsrrr<br />

VISIBLE GaD FROM SHAKING TABLE tWD PANNING<br />

cobo2jul.wri<br />

NUMBER OF GRAINS<br />

TOTAL * OF PANNINGS 16<br />

ABRADED IRREGULAR DELICATE TOTAL WON CALC V.6.<br />

SAMPLE i PANNED<br />

— —*-— —•— **""* "* "*"" ~ ""* "M"—— •——-. Hno HwwHY<br />

Y/N DIAMETER THKXNESS TPTPTP GMS PPB REMARKS<br />

BOB-87<br />

25<br />

50<br />

75<br />

75<br />

100<br />

X<br />

X<br />

X<br />

X<br />

X<br />

75<br />

75<br />

75<br />

100<br />

100<br />

10 C<br />

13 C<br />

15 C<br />

16 C<br />

20C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

COGEKA<br />

6 23.2<br />

161<br />

07/27/8'/<br />

-07 Y 25<br />

50<br />

50<br />

X<br />

X<br />

X<br />

50<br />

50<br />

75<br />

8C<br />

10 C<br />

13 C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

i<br />

EST. n PYRITE<br />

3 24.1<br />

27<br />

-08 Y 25<br />

25<br />

50<br />

50<br />

75<br />

x<br />

x<br />

x<br />

x<br />

x<br />

25<br />

75<br />

50<br />

100<br />

125<br />

5C<br />

10 C<br />

10 C<br />

15 C<br />

20C<br />

2<br />

1<br />

1<br />

1<br />

1<br />

1<br />

2<br />

1<br />

1<br />

1<br />

EST. n PYRITE<br />

6 23.3<br />

lie<br />

-09 N NO VISIBLE GOLD<br />

-10 Y 25<br />

75<br />

100<br />

x<br />

50<br />

100<br />

125<br />

8C<br />

18 C<br />

22 C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

-li Y 50<br />

50<br />

75<br />

75<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

50<br />

75<br />

75<br />

100<br />

10 C<br />

13 C<br />

15 C<br />

18 C<br />

1<br />

1<br />

1 1<br />

1 1<br />

1<br />

1<br />

2<br />

2<br />

EST. IX PYRITE<br />

3 23.7<br />

136<br />

6 21.5<br />

1BO<br />

-12 Y 50<br />

75<br />

x<br />

x<br />

100<br />

100<br />

15 C<br />

18 C<br />

1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

1<br />

1<br />

2 16.9<br />

98<br />

-13 N 100<br />

x<br />

125<br />

22 C<br />

1<br />

1<br />

1 23.4<br />

91<br />

-14 w tm vrf<br />

ffi!<br />

F mr n


1 1111I111<br />

1 111111111<br />

PAGE 3<br />

BOLD aASSIFICATION<br />

C06EHA<br />

07/27/85<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2jul.wri<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNIN6S 16<br />

ABRADED IRREGULAR DELICATE TOTAL<br />

SAMPLE K PANNED ———— ———<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

NON CALC V.6.<br />

KAR A3SAY<br />

nHO HOwnl<br />

6MS PPB REMARKS<br />

BOB-87<br />

-15 N 100 X 100<br />

20 C 1<br />

1<br />

1<br />

33,0 45<br />

-16 Y 75 X 75<br />

100 X 100<br />

100 X 125<br />

15 C 1<br />

20C 1<br />

22 C 1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

3<br />

39.5 108<br />

-17 Y 25 X 50<br />

5-) X 75<br />

75 X 100<br />

BC 1 2<br />

13 C 1 1<br />

16 C 1<br />

3<br />

2<br />

1<br />

EST. IX PYRITE<br />

6<br />

33.7 59<br />

-18 Y 25 X 50<br />

50 X 50<br />

50 X 75<br />

5d X 100<br />

75 X 100<br />

8 C 1<br />

10 C 1<br />

13 C 1<br />

15 C 1<br />

18 C 1<br />

EST. IX PYRITE<br />

5<br />

41.0 56<br />

101-01 N NO VISIBLE GOLD<br />

-02 N 75 X 125<br />

20 C 3<br />

1<br />

1<br />

26.8 56<br />

-03 N 25 X 75<br />

10 C l<br />

1<br />

1<br />

39.6 5<br />

-04 N 75 X 75<br />

15 C 1<br />

1<br />

1<br />

39.6 16<br />

-05 Y 50 X 50<br />

75 X 325<br />

100 X 150<br />

125 X 200<br />

200 X 250<br />

10 C 3<br />

20 C 1<br />

25 C 1<br />

31 C 1<br />

42 C 1<br />

3<br />

1<br />

1<br />

1<br />

1<br />

EST. 2X PYRITE<br />

7<br />

36.6 744


i 1<br />

1<br />

1<br />

1<br />

1<br />

l l<br />

1 1<br />

1 11111111<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD ROM SHAKING TABLE fIND PANNING<br />

cobo2jul.wri<br />

inifil lUIHL 8 n OF UT PAMMtKlfi*? rnliriiriui)<br />

t lo A<br />

SAMPLE S<br />

PANNED<br />

Y/N DIAMETER THIC<br />

BOB-87<br />

-06 Y 25 X 50<br />

50 X 50<br />

50 X 75<br />

125 X 200<br />

175 X 250<br />

-07 N NO VISIBLE GOLD<br />

ABRADED<br />

NUMBER OF GRAINS<br />

COGEM/ \<br />

IRREGULAR DELICATE<br />

srrrrssr rzss5ssss srsrrrrs<br />

wes T P T P T P<br />

8C 1<br />

10 C 1<br />

13 C 1<br />

31 C 1<br />

40 C 1<br />

TOTAL<br />

srrrr<br />

1<br />

1<br />

1<br />

1<br />

1<br />

5<br />

NON CALC V.6.<br />

HAG ASSAY<br />

6MS PPB REMARKS<br />

36.0 569<br />

EST. U PYRITE<br />

07/27/e:<br />

-08 Y 50 X 50<br />

50 X 75<br />

50 X 100<br />

100 X 100<br />

125 X 175<br />

10 C 1<br />

13 C 1<br />

15 C 1<br />

20C 1<br />

29C 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

EST. U PYRITE<br />

5<br />

28.9 264<br />

-09 Y 50 X 75<br />

75 X 100<br />

13 C 1 1<br />

18 C 1<br />

2<br />

1<br />

EST. IZ PYRITE<br />

3<br />

30.0 59<br />

-10 N 100 X 150<br />

25 C 1<br />

1<br />

1<br />

31.1 93<br />

-11 N NO VISIBLE GOLD<br />

-12 N 75 X 100<br />

18 C 1<br />

1<br />

1<br />

34.7 29<br />

-13 N NO VISIBLE GOLD<br />

-14 Y 25 X 50<br />

50 X 50<br />

100 X 125<br />

150 X 275<br />

8C 1<br />

10 C 1<br />

22 C 1<br />

40 C 1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

4<br />

31.1 514<br />

101-15 N NO VISIBLE GOLD


1 1111111iiiiiiiiiii<br />

PAJU<br />

COGEMA<br />

07/30/87<br />

•"<br />

SOLD CLASSIFICATION<br />

VISIBLE BOLD FROM SHAKING TABLE AND PAWING<br />

COB03JUL.KR1<br />

TOTAL t OF PANNINSS 8 ———<br />

ABRADED<br />

SAMPLE t PANNED =======<br />

Y/N DIAMETER THICKNESS T<br />

BOB-87<br />

102-01 N NO VISIBLE GOLD<br />

-02 N 275 X 275 50 C 1<br />

-03 N 75 X 150 22 C 1<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 Y 25 X 50 8 C<br />

25 X 75 10 C<br />

50 X 50 10 C<br />

75 X 100 18 C 1<br />

100 X 150 25 C 1<br />

150 X 200 34 C 1<br />

-07 N NO VISIBLE GOLD<br />

-08 N 100 X 125 22 C 1<br />

-09 N 100 X 200 29 C 1<br />

•-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

103-01 N 50 X 75 13 C 1<br />

-02 Y 25 X 25 5 C<br />

50 X 50 10 C 1<br />

NUMBER OF GRAINS<br />

1<br />

1<br />

IRREGULAR DELICATE TOTAL<br />

1<br />

rsrrzzsss ssssssss srrrr<br />

NON<br />

HAG<br />

CALC V.G.<br />

ASSAY<br />

P T P ' T P 6MS PPB 1REMARKS<br />

1<br />

1 19.3 1475<br />

1<br />

1 19.9 107<br />

2 2<br />

1EST. 27. PYRITE<br />

1 1<br />

2 2<br />

1<br />

1<br />

1<br />

e 35.6 348<br />

3<br />

1 25.7 83<br />

1<br />

1 27.3 181<br />

1<br />

1 26.6 14<br />

s<br />

EST. Vi. PYRITE<br />

l GRAIN GALENA


1 1111I1I111I111<br />

P|fe?<br />

COGEMA<br />

07/30/87<br />

GOLD CLASSIFICATION'<br />

VISIBLE GOLD FROH SHAKING<br />

TABLE AND PANNING<br />

COB03JUL.WRI<br />

NUMBER OF GRAINS<br />

TOTAL 1 OF PANNING<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE it PANNED ———— ——--B- *B-BB*-B -.-*s Tltm HODMI<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REHARKS<br />

BOB-87<br />

50 X<br />

50 X<br />

75 X<br />

75 13 C 1 1<br />

75 50 M 1 1<br />

75 15 C 1 1<br />

5 24.7 109<br />

-03 Y 25 X<br />

50 X<br />

75 X<br />

175 X<br />

25 5 C 1 1 EST. IX PYRITE<br />

50 10 C 1 1<br />

125 20 C 1 1<br />

300 44 C 1 1<br />

4 23.0 888<br />

-04 Y 50 X<br />

75 X<br />

100 X<br />

75 13 C 1 1 EST. 1). PYRITE<br />

100 18 C 1 1<br />

100 20 C 1 1<br />

3 23.0 125<br />

-05 N 125 X<br />

175 29 C 1 1<br />

1 16.8 294<br />

-06 N 125 X<br />

150 27 C 1 1<br />

1 16.3 235<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

1<br />

1<br />

1<br />

-10 N NO VISIBLE GOLD -<br />

-11 N 125 X 175 29 C 1 1<br />

1 26.0 190<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

1 -15 N NO VISIBLE GOLD


1 111II<br />

1<br />

1<br />

I<br />

1<br />

1<br />

1I<br />

I<br />

1t<br />

1<br />

1<br />

I 1<br />

BOB-87<br />

-16 N NO VISIBLE BOLD<br />

-17 N NO VISIBLE GOLD<br />

104-01 N NO VISIBLE GOLD<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 Y 50 X 50 10 C 1<br />

75 X 75 15 C<br />

125 X 125 25 C 1<br />

-06 Y 25 X 50 BC<br />

5(i X 50 10 C<br />

50 X 75 13 C 2<br />

-07 Y 25 X 25 5 C<br />

25 X 50 BC<br />

50 X 50 10 C 1<br />

75 X 125 20 C l'<br />

-OS N 75 X 75 15 C 1<br />

-09 N NO VISIBLE GOLD<br />

104-10 Y 25 X 50 8 C<br />

50 X 50 10 C !<br />

50 X 100 15 C<br />

75 X 75 15 C 1<br />

100 X 100 20 C 1<br />

3 4 EST. IX<br />

1 1<br />

1<br />

6 25.1 171<br />

2 1 3 EST, 21<br />

2 2<br />

2<br />

7 28.2 49<br />

1 1 EST. U<br />

1 1<br />

1<br />

1<br />

4 26.0 69<br />

1<br />

1 20.3 32<br />

1 1 EST. IX<br />

1<br />

1 1<br />

1<br />

1<br />

5 29.3 104<br />

-<br />

PYRITE<br />

PYRITE<br />

PYRITE<br />

PYRITE<br />

PA0<br />

COGEMA<br />

07/30/67<br />

GOLD CLASSIFICATION.<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB03JUL.WRI<br />

NUMBER OF GRAINS<br />

TOTAL i OF PANNINGS 8 ————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE * PANNED sssrsrrr assss —————— "— rsrrrsrz ——— -"— -* rssrr ———— MAR imu AtRAY r13wni<br />

Y/N DIAMETER THICKNESS T P T P T P GMS PPB REMARKS


GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE A® PANNING<br />

COGEMA<br />

C0304JUL.WRI<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNINGS 10<br />

ABRADED IRREGULAR DELICATE TOTAL<br />

SAMPLE S PANNED ————: rcrssrzss srrrsszs szzrs<br />

V/N DIAMETER THICKNESS T P T P T P<br />

BOB-87<br />

104-11 N NO VISIBLE GOLD<br />

NQN<br />

MAR<br />

i frju<br />

CALC V.6.<br />

ACCAV<br />

riwvn i<br />

6MS PPB REMARKS<br />

08/04/67<br />

-12 N NO VISIBLE GOLD<br />

1 1<br />

1<br />

1<br />

1<br />

1 m<br />

I<br />

-13 N 75 X 100<br />

18 C 1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

i<br />

I<br />

1<br />

I<br />

i<br />

1<br />

1<br />

-14 Y 50 X 50<br />

100 X 150<br />

175 X 200<br />

-15 N 200 X 475<br />

-16 N 75 X 100<br />

-17 N NO VISIBLE 60LD<br />

-18 Y 25 X 50<br />

50 X 50<br />

50 X 75<br />

50 X 100<br />

ICKi X 125<br />

175 X 300<br />

-1? Y 50 X 50<br />

50 X 75<br />

105-01 Y 75 X 100<br />

150 X 275<br />

150 X 325<br />

200 X 325<br />

-02 N WO V1S1SLE BOLD<br />

10 C<br />

25C 1<br />

36 C 1<br />

59 C 1<br />

18 C 1<br />

8C<br />

10 C<br />

13 C<br />

15 C<br />

22 C 1<br />

44 C 1<br />

10 C<br />

13 C 1<br />

18 C<br />

40 C i<br />

44 C 1<br />

46 C 1<br />

1 1<br />

1<br />

1<br />

1 1<br />

1 1<br />

2 2<br />

1 1<br />

1<br />

1<br />

1 1<br />

1<br />

1 1<br />

1<br />

1<br />

1<br />

-<br />

1<br />

3<br />

1<br />

1<br />

I<br />

1<br />

7<br />

2<br />

4<br />

44.1 23<br />

EST. 27. PYRITE<br />

31.9 393<br />

37.9 1341<br />

25.3 . 40<br />

EST. \l PYRITE<br />

32.0 703<br />

EST. IX PYRITE<br />

36.0 16<br />

EST. IX PYRITE<br />

31.1 1873


l 111l1l1i11l11111i1<br />

F*<br />

COGEMA<br />

08/04/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04JUL.WRI<br />

NUMBER OF GRAINS<br />

TOTAL f OF PANNINGS 10 ———<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

QAMPi P 1 PANIJCTi ———— -. .—————————— r ——-———— s ———— UAP AQCAV<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-03 N 75 X 100 16 C 1<br />

1<br />

1 33.1 31<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 Y 50 X 50 10 C 1<br />

50 X 100 15 C 1<br />

75 X 75 15 C<br />

-07 Y 50 X 75 13 C<br />

100 X 100 20 C 1<br />

200 X 300 46 C 1<br />

-08 N NO VISIBLE GOLD<br />

106-01 N NO VISIBLE GOLD<br />

-02 N 50 X 75 13 C 1<br />

-03 N NO VISIBLE GOLD<br />

-04 Y 25 X 25 5 C<br />

50 X 50 10 C 1<br />

50 X 75 13 C<br />

75 X 75 15 C 2<br />

-05 Y 25 X 50 8 C<br />

50 X 75 13 C 1<br />

50 X 100 15 C 1<br />

75 X 75 75 M<br />

-06 Y 50 X 75 13 C 2<br />

1 EST. n<br />

l<br />

1 1<br />

3 33.9 43<br />

1 1 EST. 27.<br />

1<br />

1<br />

3 37.3 631<br />

1<br />

1 25.9 14<br />

1 1 EST. 17.<br />

1<br />

1 1<br />

2<br />

5 21.6 87<br />

1 1 EST. IX<br />

1<br />

1<br />

1 1<br />

4 21.5 198<br />

1 3 EST. IX<br />

10.3 Ki9-<br />

PYRITE<br />

PYRITE<br />

PYRITE<br />

PYRITE<br />

PYRITE


l<br />

l<br />

l<br />

C06EHA . 08/04/8?<br />

GOLD CLASSIFICATION<br />

lI<br />

I<br />

VISIBLE GOLD FROM SHAKING TABLE ftND PANNIN6<br />

COB04JUL.WRI<br />

NUMBER OF'GRAINS<br />

TOTAL * Or PnNNINbS lv "~~~~~" mL""""~~— *L—————w..--*——— —-——-<br />

SAMPLE f PANNED<br />

ABRADED IRREGULAR DELICATE TOTAL NON<br />

^^^ ^^srr ^^^ rrsES HAG<br />

CALC V.G.<br />

ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-07 N HO VISIBLE GOLD<br />

V<br />

l<br />

i ll<br />

-09 N 100 X 100 20 C l l<br />

l 24.9 60<br />

-10 N 75 X 100 18 C l l<br />

l 20.0 51<br />

-11 N m VISIBLE BOLD<br />

-12 N NO VISIBLE GOLD ,<br />

-OB N NO VISIBLE GOLD<br />

-13 ' N NO VISIBLE GOLD<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

-14 N NO VISIBLE GOLD<br />

-15 N NO VISIBLE GOLD<br />

-16 N 100 X 175 27 C l l<br />

-17 N NO VISIBLE GOLD<br />

l 25.7 149<br />

-!B Y 25 X 25 5 C l l EST. li PYRITE<br />

25 X 50 6 C 2 2<br />

50 X 50 10 C l l<br />

100 X 125 22 C l l<br />

125 X 200 31 C l l<br />

6 27.5 316<br />

107-01 N NO VISIBLE GOLD<br />

i l<br />

-03 N S X 75 10 C l ' l<br />

l 34.0<br />

-02 N NO VISIBLE GOLD<br />

-W N HO VISIBLE GOLD


l l<br />

l<br />

l l<br />

l<br />

l l<br />

l l<br />

l f<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

60LD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COSEHA 08/04/87<br />

COKHJUL.WRI<br />

NUMBER OF BRAINS<br />

TOTAL i OF PANNIN65 10 ———————————————-———<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE * PANNED ~~~: ^^^ ^^^ KSSS fjAB ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6M5 PPB REMARKS<br />

BOB-87<br />

107-05 N NO VISIBLE GOLD


1 111111111111111111<br />

COGEMA 06/07/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB01AUG.WRI<br />

TOTAL It OF PANNINGS 16<br />

SAMF1E i<br />

NUMBER OF BRAINS<br />

ABRADED IRREGULAR DELICATE<br />

PANNED<br />

rrzrzssz sssssssss ssssssss<br />

V/h DIAMETER THICKNESS T PT P T P<br />

TOTAL<br />

rssss<br />

WON CALC V.6.<br />

MAG ASSAY<br />

GMS PPB REMARKS<br />

BOB-8?<br />

107-06 N 375 X 400<br />

66 C 1<br />

1<br />

1<br />

21.6 3460<br />

-07 N NO VISIBLE GOLD<br />

-03 Y 25 X 50<br />

50 X 50<br />

50 X 75<br />

75 X 100<br />

8C 2<br />

10 C 1<br />

13 C 1 1<br />

18 C 1<br />

EST. IX PYRITE<br />

2<br />

1<br />

2<br />

1<br />

6<br />

24.0 88<br />

-0? Y 25 X 50<br />

50 X 75<br />

75 X 100<br />

100 X 150<br />

8C 1<br />

13 C 1<br />

18 C 1<br />

25 C 1<br />

1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

4<br />

22.9 190<br />

-10 Y 25 X 25<br />

25 X 75<br />

50 X 75<br />

75 A 100<br />

5C 1<br />

10 C 1 1<br />

13 C 2<br />

18 C 1<br />

1<br />

2<br />

2<br />

1<br />

EST. IX PYRITE<br />

6<br />

19.9 109<br />

-11 N 50 X 150<br />

20 C 1<br />

1<br />

1<br />

17.1 88<br />

-12 N 75 X 75<br />

15 C 1<br />

1<br />

1<br />

18.5 35<br />

-13 Y 25 X 75<br />

50 X 50<br />

50 X 75<br />

75 X 125<br />

10 C 1<br />

10 C 1<br />

13 C 1<br />

20 C 1<br />

1<br />

1<br />

1<br />

1<br />

EST. 17. PYRITE<br />

4<br />

17.4 130<br />

-14 N 50 x 100<br />

15 C 1<br />

1<br />

1<br />

16.1 40<br />

-15 Y 50 X 50<br />

10 C 1 t<br />

2<br />

EST. 0.5X PYRITE


1 111llw<br />

1 111<br />

1 I1111111<br />

P AA<br />

COGEHA<br />

08/07/67<br />

GOLD CLASSIFICATION<br />

VISIBLE SOLD FROh SHAKING TfiBLE AND PANNING<br />

*<br />

DDK'1 AUG. WR1<br />

TOTftL ft OF PANNINSS 16<br />

NUMBER OF GRAINS<br />

——— -<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

S&MPI F tt PfiMl^n rrsrssr: : ssssssssr ssssss.. ssrss fiftg flSSAY<br />

Y/N DIAMETER THICKNESS T P T P T P QMS PPB REMARKS<br />

BOB-87<br />

50 X 75 !3 C<br />

i 1<br />

3 20.3 37<br />

-16 H NO VISIBLE GOLD<br />

-17 N 100 X 125 22 C 1<br />

1<br />

1 21.1 101<br />

-IB N 50 X 100 15 C 1<br />

1<br />

1 28.0 23<br />

-19 N 100 X 100 20 C 1<br />

1<br />

1 33.9 44<br />

-20 N 75 X 75 15 C 1<br />

1<br />

1 40.2 16<br />

-21 N 50 X 100 15 C 1<br />

1<br />

1 29.4 22<br />

-22 V 25 X 50 6 C<br />

25 X 75 10 C<br />

50 X 50 10 C<br />

50 X 75 13 C<br />

75 X 100 18 C 1<br />

75 A 125 20 C 1<br />

100 X 125 22 C 1<br />

2 2 EST. 22 PYRITE<br />

2 2<br />

1 1<br />

1 1<br />

i1<br />

1<br />

9 27.2 211<br />

108-01 V 25 X 50 S C<br />

50 X 75 13 C 1<br />

125 X 150 27 C i<br />

175 X 325 46 C 1<br />

1 1 EST. 52 PYRITE<br />

1<br />

1<br />

1<br />

4 35. B 725<br />

-02 N 75 X 500 13 C 1<br />

1<br />

1 30.2 33


l 11<br />

1 1l1111111111111<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PftNNINo<br />

CQ6EMA<br />

08/07/87<br />

CQB01AU6.MR1<br />

NUMBER OF GRAINS<br />

TOTAL t OF PANNIN83 16<br />

ABRADED IRREGULAR DELICATE<br />

SAMPLE ft PANNED<br />

srrcrrrr crrrrsrsr ssssss::<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

TOTAL m CALC V.6.<br />

rrrrr MAQ ASSAY<br />

GMS PPB REMARKS<br />

BOB-67<br />

-03 Y 25 X 50<br />

75 X 75<br />

75 X 100<br />

-04 Y 25 X 25<br />

25 X 50<br />

50 X 75<br />

50 X 100<br />

75 X 100<br />

-05 Y 25 X 25<br />

100 X 150<br />

-06 V 25 X 25<br />

50 X 50<br />

50 X 75<br />

75 X 75<br />

100 X 150<br />

-07 Y 25 X 25<br />

25 X 50<br />

50 X 75<br />

50 X 125<br />

100 X 150<br />

100 X 175<br />

-08 N 50 X 50<br />

: -09 N NO VISIBLE GOLD<br />

-10 Y 25 X<br />

50 X<br />

75<br />

50<br />

50 l 75<br />

100 X 150<br />

BC 1<br />

15 C 1<br />

18 C 1<br />

5C 1<br />

8C 1<br />

13 C 2<br />

15 C I<br />

18 C 1<br />

5 C 1<br />

25C 2<br />

5C 1<br />

10 C 2<br />

13 C 1<br />

15 C i<br />

25 C 1<br />

5 C 1<br />

8C 1<br />

13 C 1<br />

16 C 1<br />

25 C 1<br />

27 C 1<br />

10 C 1<br />

10 C<br />

10 C 1<br />

1<br />

!3 C 1<br />

25 C 1<br />

1 EST. 0.5X PYRITE<br />

1<br />

1<br />

3 23.0 75<br />

1 EST. 27. PYRITE<br />

1<br />

2<br />

I<br />

1<br />

6 27.0 93<br />

1 NO SULPHIDES<br />

2<br />

3 27.7 210<br />

1 EST. 10 GRAINS PYRITE<br />

2<br />

1<br />

1<br />

1<br />

6 23.9 181<br />

1 EST. IX PYRITE<br />

1<br />

1<br />

1<br />

1<br />

1<br />

6 26.6 306<br />

1<br />

1 27.7 7<br />

1 EST. IX PYRITE<br />

1<br />

1<br />

1


1<br />

111111111111111111<br />

PA^fc<br />

C06EMA 08/07/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

CGBOlAUG.tJRl<br />

TOTAL i OF PANNINSS 16<br />

' NUMBER OF GRAINS<br />

~ — ~<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SfiPtPI F ft PAUMPR zzsszsr E sss —— sss sss — s — srszs Mfifl tfiKM<br />

Y/N DIAMETER THICKNESS T P T P t P GMS PPB REMARKS<br />

BOB-87<br />

4 24.0 152<br />

-11 N NO VISIBLE GOLD<br />

-12 Y' 25 X 50 8 C<br />

25 X 100 13 C 1<br />

50 X 75 13 C 1<br />

125 X 175 29 C<br />

2 2 EST. 17. PYRITE<br />

1<br />

1<br />

1 1<br />

5 19.1 306<br />

-13 N NO VISIBLE GOLD<br />

109-01 N 75 X 100 18 C 1<br />

1<br />

t 24.1 42<br />

-02 N 50 X 75 13 C 1<br />

1<br />

1 20.4 18<br />

-03 Y 50 X 50 10 C l<br />

100 X 100 20 C<br />

-3 4 EST. 17. PYRITE<br />

1 1<br />

5 21.6 105<br />

-04 Y 25 X 25 5 C<br />

25 X 50 BC<br />

50 X 50 10 C<br />

50 X 75 13 C<br />

75 X 100 18 C 1<br />

1 1 ESI. 17. PYRITE<br />

i 1<br />

1 1<br />

1 1<br />

1 2<br />

6 19.4 139<br />

-05 N NO VISIBLE GOLD<br />

-06 N 125 X 125 25 C 1<br />

•'<br />

1<br />

1 17.6 164<br />

-07 N NO VISIBLE GOLD<br />

-08 N 75 X /'5 15 C 1<br />

i<br />

1 24.5 26<br />

-09 N 50 X 75 13 C 1<br />

i


l l<br />

l l<br />

l<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEMA 08/07/87<br />

COB01AU6.WRI<br />

NUMBER OF GRAINS<br />

TOTAL S OF CANNINGS 16 ~——————-————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMFtE i PANNEfl ^^^ ^^.^ *^s^ SZSrr HAG ASSAY<br />

Y/fl DIAMETER THICKNESS T P T P T P CMS FPB REMARKS<br />

BOS-&7<br />

l 22.1 l?<br />

l<br />

l<br />

109-10 N NO VISIBLE GOLD<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l


PAGE 1<br />

COGEMA<br />

08/10/87<br />

1 111111111111111111<br />

BOLD aASSIFICATION<br />

VISIBLE BOLD FROM SHAKING TABLE AND PANNINS<br />

cobo2aug.Hrl<br />

NUMBER OF BRAINS<br />

TfiTAi lUIHL v i nr Ur r.Avumtrr rHWuNob nV '———"———————— ~— ————-———<br />

SAMPLE 1 PANNED<br />

ABRADED<br />

IRRE6ULAR DELICATE TOTAL<br />

rrrrrrrs errrrsrrs srrssrrr errs:<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

BOB-87<br />

109-11 N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N 50 X 100 15 C 1 1<br />

NON<br />

MAG<br />

6MS<br />

CALC V.6.<br />

ASSAY<br />

PPB<br />

1<br />

25.9 25<br />

-15 N 100 X 125 22 C 1 1<br />

1<br />

25.9 82<br />

-16 N 50 X 75 13 C 1 1<br />

1<br />

27.3 14<br />

-17 N NO VISIBLE GOLD<br />

-18 N 50 X 75 13 C 1 1<br />

1<br />

33.7 11<br />

-19 Y 25 X 25 5 C 1 1<br />

50 X 75 13 C 2 2<br />

100 X 100 20 C 1 1 2<br />

EST. IX PYRITE<br />

5<br />

24.5 154<br />

110-01 Y 100 X 125 22 C 2 2<br />

EST. IX PYRITE<br />

2<br />

46.7 91<br />

-02 N 100 X 200 29 C 1 1<br />

1<br />

34.2 144<br />

-03 Y 75 X 225 29 C 1 1<br />

250 X 300 50C 1 1<br />

EST. IX PYRITE<br />

2<br />

24.9 1341<br />

-04 N 50 X 100 15 C 1 1<br />

1<br />

16.4 39


l l<br />

l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

PAGE 2<br />

GOLD CLASSIFICATION<br />

rssss-:——.—azssssss<br />

VISIBLE GOLD FROM SHAKING TftBLE AND PANNING<br />

tobo2aug.wri<br />

TOTAL l OF PANNIN6S 9 ——<br />

ABRADED<br />

SAMPLE l PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

N<br />

250 X 275<br />

NO VISIBLE GOLD<br />

Y 25 X 50<br />

125 X 125<br />

175 X 200<br />

N<br />

111-01 N<br />

-02<br />

N<br />

NO VISIBLE GOLD<br />

50 X 50<br />

50 X 75<br />

50 X 100<br />

75 X 100<br />

75 X . 125<br />

100 X 200<br />

NO VISIBLE GOLD<br />

50 X 75<br />

75 X 125<br />

50 X 75<br />

75 X 100<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

48C<br />

N 125 X 175 29 C<br />

BC<br />

25C<br />

36C<br />

10 C<br />

13 C<br />

15 C<br />

18 C<br />

20C<br />

29C<br />

l<br />

13 C l<br />

20 C l<br />

13 C<br />

18 C<br />

NUMBER OF GRAINS<br />

C06EMA 08/10/87<br />

IRREGULAR DELICATE TOTAL NON<br />

GMS<br />

l 29.6<br />

l 34.B<br />

2<br />

l<br />

l<br />

4 28.0<br />

6 51.5<br />

l<br />

l 14.3<br />

l<br />

l 32,3<br />

l<br />

l<br />

2 30.3<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

842<br />

142<br />

447<br />

168<br />

26<br />

46<br />

46<br />

EST. IX PYRITE<br />

EST. IX PYRITE<br />

EST. IX PYRITE


1 111111111111111111<br />

PftGE3<br />

COGEMA<br />

08/JO/B7<br />

SOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

cobo2aug.wri<br />

NUMBER OF GRAINS<br />

WTAI lUlnL t M IV Ur rHNrUNoO nAtHltkVY* Y O<br />

'—-~—— ~~ —"""•"•' - ---- - -<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE It PANNED rarsssss enm sxrrsr^ *^HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-06 N 75 X 125 20 C 1<br />

1<br />

1 22.4 67<br />

-07 N 75 X 100 18 C 1<br />

1<br />

1 26.7 38<br />

-08 N NO VISIBLE GOLD<br />

-09 N NO VISIBLE GOLD<br />

-10 Y 25 X 25 5 C 2<br />

25 X 100 13 C 1<br />

50 X 75 13 C 1<br />

50 X 100 15 C 1<br />

75 X 100 18 C 1<br />

2 EST. 1Z PYRITE<br />

1<br />

1<br />

1<br />

1<br />

6 29.4 83<br />

-11 N NO VISIBLE GOLD<br />

112-01 N 100 X 150 25 C 1<br />

1<br />

1 34.2 65<br />

-02 N NO VISIBLE GOLD<br />

-03 Y 25 X 50 8 C 1<br />

50 X 75 13 C 1<br />

50 X 100 15 C 1<br />

75 X 125 20 C 1<br />

1 EST. 2X PYRITE<br />

1<br />

1<br />

1<br />

4 31.6 82<br />

-04 Y 50 X 75 13 C 1<br />

75 X 100 18 C 1 1<br />

100 X 125 22 C 1<br />

1 EST. 2X PYRITE<br />

2<br />

1<br />

4 32.1 141<br />

-05 N 75 X 75 15 C 1<br />

I<br />

1 18.7 34<br />

-06 N NO VISIBLE GOLD


l PAGE 4 COGEMA OB/10/87<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

GOLD CLASSIFICATION<br />

' VISIBLE BOLD FROM SHAKING TABLE AM) PANNING<br />

cobo2aug.Hri<br />

NUMBER OF BRAINS<br />

TOTAL t OF PAKNIN6S 9 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SAMPLE l PANNED zz^rrr :———— ———— ssrss HAG ASSAY<br />

BOB-87<br />

Y/N DIAMETER THICKNESS TPTPTP 6MS PPB REMARKS<br />

113-01 N NO VISIBLE GOLD<br />

113-02 N NO VISIBLE GOLD


1<br />

1111I•i'<br />

FW<br />

COGEMA<br />

08/13/87<br />

BOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB03AUG.WRI<br />

TOTAL # OF PANNINGS 13 ————<br />

ABRADED<br />

CAMpj f f pfiHMCn ———— E-. ——————— sss —— j-.-- —— ————— MAC fllSOY<br />

Y/N DIAMETER THICKNESS T<br />

NUMBER OF GRAINS<br />

IRREGULAR DELICATE TOTAL WON<br />

CALC V.G.<br />

P T P T P 6MS Pf'B REMARKS<br />

1 111111111111<br />

BOB-87<br />

113-03 N 75 X 75 15 C 1<br />

-04 Y 100 X 125 22 C 1<br />

150 X 200 34 C 1<br />

-05 N NO VISIBLE GOLD<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE GOLD<br />

-08 N 50 X 75 13 C 1<br />

-09 N 50 X 50 10 C 1<br />

-10 N NO VISIBLE GOLD<br />

-11 N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

114-01 Y 25 X 25 5 C 1<br />

50 X 50 10 C<br />

50 X 75 13 C 1<br />

75 X 100 18 C<br />

-02 N 50 X 100 15 C 1<br />

-03 Y 25 X 50 BC<br />

50 X 50 10 C<br />

50 X 75 13 C 1<br />

75 X 100 18 C 1<br />

100 X 100 20 C 1<br />

••"<br />

1<br />

1 33.6 19<br />

1 EST. IX PYRITE<br />

1<br />

2 20.3 486<br />

1<br />

1 24.7 15<br />

1<br />

1 21.9 9<br />

1 EST. 3X PYRITE<br />

1 1<br />

1<br />

1 1<br />

4 30.3 53<br />

1<br />

1 29.0 22<br />

1 1 EST. 2X PYRITE<br />

2 2<br />

1<br />

1<br />

1<br />

32.3 104


l l l<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PAWING<br />

COGEMA 08/13/87<br />

1<br />

COB03AU6.WRI<br />

UIHL * UT rHWIirao<br />

NUMBER OF GRAINS<br />

ij ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

l h SAMPLE t PANNED<br />

•——"— ~— ——- nnu M^JMI<br />

Y/N DIAMETER THICKNESS T P T P TP BUS PPB REMARKS<br />

I<br />

1<br />

111111111ii1<br />

BOB-87<br />

-04 Y 50<br />

50<br />

100<br />

100<br />

X<br />

X<br />

X<br />

X<br />

50<br />

100<br />

100<br />

200<br />

10 C<br />

15 C<br />

20C<br />

29C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

EST. 3'/. PYRITE<br />

4 33.8<br />

215<br />

-05 N 75<br />

X<br />

100<br />

18 C<br />

1<br />

1 .<br />

1 31.4<br />

32<br />

-06 N 50<br />

x<br />

100<br />

15 C<br />

1<br />

1<br />

1 38.5<br />

17<br />

-07 N 125<br />

x<br />

150<br />

27 C<br />

1<br />

1<br />

1 26.3<br />

145<br />

-08 N 50<br />

x<br />

75<br />

13 C<br />

1<br />

1<br />

1 26.1<br />

14<br />

-09 Y 25<br />

50<br />

175<br />

250<br />

25<br />

75<br />

375<br />

275<br />

5C<br />

13 C<br />

42 C<br />

48 C<br />

1<br />

1<br />

1<br />

1<br />

EST. IX PYRITE<br />

-10 Y 50.<br />

50<br />

75<br />

100<br />

125<br />

125<br />

125<br />

200<br />

x<br />

x<br />

x<br />

x<br />

x<br />

xxx<br />

21.0<br />

2561<br />

x<br />

x<br />

x<br />

x<br />

50<br />

75<br />

125<br />

125<br />

175<br />

200<br />

225<br />

200<br />

10 C<br />

13 C<br />

20C<br />

22C<br />

29C<br />

31 C<br />

34 C<br />

38C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

I<br />

EST. 0.5Z PYRITE<br />

B 34.3<br />

1006<br />

-11 Y 75<br />

125<br />

175<br />

x<br />

x<br />

x<br />

100<br />

125<br />

275<br />

18 C<br />

25 C<br />

42 C<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

EST. 0.5X PYRITE<br />

3 25.1 794


1<br />

1<br />

1<br />

111<br />

1<br />

111111<br />

i<br />

iiiii<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING' TABLE AND PANNING<br />

COGEMA 08/13/87<br />

CQB03AU6.WRI<br />

TOTAL 1 OF PANNINGS 13<br />

SAMPLE * PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

NUMBER OF ERAINS<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

a.—- .a-i-n-jiT-i—<br />

^~"-" —' m~wmim<br />

**"**"<br />

*PW———— ^.^— M~HB MAC<br />

*"*""* fc*-***w flHu<br />

ACOAV<br />

HwdHT<br />

TPTPTP 6MS PPB REMARKS<br />

-12 Y 25 X 50<br />

50 X 75<br />

150 X 175<br />

175 X 200<br />

200 X 300<br />

8C<br />

13 C<br />

31 C<br />

36C<br />

46 C<br />

1 1 EST. 1Z<br />

1 1 2<br />

1 1<br />

1 1<br />

1 1<br />

PYRITE<br />

6 31.4 1216<br />

-13 Y 50 X 100<br />

75 X 100<br />

75 X 125<br />

100 X 150<br />

15 C<br />

18 C<br />

20C<br />

25C<br />

1 1 EST. IX<br />

1 1<br />

1 1<br />

1 1<br />

PYRITE<br />

4 29.9 202<br />

115-01 N NO VISIBLE GOLD<br />

-02 Y 50 X 50<br />

50 X 75<br />

75 X 100<br />

150 X 275<br />

10 C<br />

13 C<br />

18 D<br />

40 C<br />

1 1 EST. 2X<br />

1 1<br />

1 1<br />

1 1<br />

PYRITE<br />

4 36.5 415<br />

-03 N 75 X 75<br />

15 C<br />

1 1<br />

1 36.7 17<br />

-04 N 150 X 225<br />

36 C<br />

1 1<br />

1 34.8 272<br />

-05 Y 50 X 50<br />

50 X 75<br />

50 X 100<br />

75 X 75<br />

75 X 100<br />

100 X 150<br />

10 C<br />

13 C<br />

15 C<br />

15 C<br />

18 C<br />

25C<br />

2 2 EST. 2Z<br />

1 1<br />

1 1<br />

1 1<br />

1 1<br />

1 1<br />

7 33.4 178<br />

PYRITE<br />

-06 N 100 X 100<br />

20 C<br />

1 1<br />

1 27.5 55<br />

-07 N NO VISIBLE BOLD


l l<br />

l<br />

l l<br />

l<br />

l l l<br />

l l<br />

l<br />

l l<br />

l<br />

l l<br />

l<br />

l<br />

GOLD aASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TftBLE AND FANNING<br />

COGEMA 08/13/87<br />

COB03AUG.WRI<br />

NUMBER OF BRAINS<br />

TOTAL l OF PANNINGS 13<br />

ABRADED IRREGULAR DELICATE TOTAL NOM CALC V.G.<br />

SAMPLE It PANNED<br />

AG ASSAY<br />

Y/N DIAMETER THICKNESS<br />

6MS PPB REMARKS<br />

B-87<br />

-09 N<br />

50 X 75<br />

75 X 75<br />

75 X 150<br />

150 X 225<br />

-10 N NO VISIBLE BOLD<br />

-11 N NO VISIBLE GOLD<br />

-12 N NO VISIBLE GOLD<br />

-13 N NO VISIBLE GOLD<br />

-14 N NO VISIBLE GOLD<br />

-15 N<br />

-16 N<br />

115-17 Y<br />

150 X 200<br />

] VISIBLE GOLD<br />

75 X 100<br />

150 X 225<br />

13 C<br />

15 C<br />

22C<br />

36C<br />

34C<br />

18 C<br />

36C<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

4 26.3<br />

l<br />

l 23.8<br />

l 26.6<br />

2 20.6<br />

133<br />

397<br />

291<br />

508<br />

EST. U PYRITE<br />

EST. IX PYRITE<br />

0.5X CHALCOPYRITE


1 1<br />

1 111<br />

1<br />

PAG^<br />

GOLD aASSIFICATION<br />

COGEHA<br />

08/14/87<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04AUG.WRI<br />

NUHBER OF GRAINS<br />

TOTAL 1 OF PANNIN6S 10 ————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL<br />

SAMPLE t PANNED Errrrrrr rrrrrrrrs rzrr.r^ SSESS<br />

Y/N DIAMETER THICKNESS T P T P T P<br />

NON<br />

HAG<br />

6MS<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

BOB-87<br />

116-01 N 75 X 100 18 C 1<br />

1<br />

1<br />

55.1 29<br />

-02 Y 75 X 75 15 C 1<br />

325 X 625 77 C 1<br />

1<br />

1<br />

EST. 5Z PYRITE<br />

1 11111111111<br />

-03 N NO VISIBLE GOLD<br />

2<br />

45.9 2860<br />

-04 N 75 X 100 IB C 1<br />

1<br />

1<br />

12.9 78<br />

117-01 Y 50 X 50 10 C 1<br />

50 X 100 15 C 1<br />

75 X 100 18 C 2<br />

1<br />

1<br />

2<br />

EST. U PYRITE<br />

4<br />

15.8 181<br />

-02 N 225 X 300 18 C 1<br />

1<br />

1<br />

8.1 3077<br />

-03 Y 25 X 50 8 C 1<br />

50 X 50 10 C 2<br />

75 X 100 18 C 1<br />

75 X 125 20 C 1<br />

125 X 300 40 C 1<br />

1<br />

2<br />

1<br />

1<br />

1<br />

EST. n PYRITE<br />

6<br />

20.5 808<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

118-01 N 50 X 75 13 C 1<br />

1<br />

1<br />

34.4 li<br />

-02 N NO VISIBLE GOLD<br />

-03 N 75 X 100 18 C 1<br />

1<br />

1<br />

29.7 34


1 111l1<br />

1 1<br />

1<br />

GOLD CLASSIFICATION<br />

COGEttA<br />

08/14/87<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB04AUG.WRI<br />

NUMBER OF GRAINS<br />

TOTAL 1 OF CANNINGS 10<br />

SAMPLE K PANNED<br />

ABRADED<br />

csssrss'1: IRREGULAR DELICATE TOTAL NON<br />

trssterc rrrrsrsr s^r MAG<br />

CALC V.G.<br />

ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-04 Y 25 X 50<br />

50 X 50<br />

50 X 75<br />

100 X 125<br />

200 X 325<br />

BC<br />

10 C<br />

13 C<br />

22 C 1<br />

48 C 1<br />

1 1 EST. 27.<br />

2 2<br />

1 1<br />

1<br />

1<br />

PYRITE<br />

6 31.5 885<br />

-05 N 50 X 75<br />

13 C 1<br />

1<br />

1 26.4 14<br />

-06 N NO VISIBLE GOLD<br />

1 11<br />

1 111111<br />

-07 Y 50 X 50<br />

50 X 75<br />

100 X 125<br />

10 C 1<br />

13 C 1<br />

22C<br />

1 EST. 2Z<br />

1<br />

1 1<br />

PYRITE<br />

3 22.0 122<br />

119-01 Y 25 X 50<br />

50 X 75<br />

75 X 100<br />

8C<br />

13 C 1<br />

IB C 1<br />

1 1 EST. 2Z<br />

1<br />

1<br />

PYRITE<br />

3 33.9 43<br />

120-01 Y 50 X 50<br />

50 X 100<br />

75 X 100<br />

75 X 125<br />

10 C 1<br />

15 C<br />

18 C<br />

20C 1<br />

1 EST. 3X<br />

1 1<br />

1 1<br />

1<br />

PYRITE<br />

4 37.7 B9<br />

121-01 Y 25 X 25<br />

25 X 50<br />

50 X 50<br />

50 X 75<br />

50 X 100<br />

75 X 75<br />

75 X 100<br />

100 X 100<br />

5C<br />

8C<br />

10 C<br />

13 C<br />

15 C 1<br />

15 C 1<br />

18 C 1<br />

20C<br />

1 1 EST. 3X<br />

2 2<br />

1<br />

1<br />

1<br />

PYRITE<br />

9 32.9 138<br />

122-01 N 125 X 175<br />

29 C 1<br />

1<br />

1 34.8 134


l 1<br />

1<br />

PAGE3<br />

BOLD CLASSIFICATION<br />

rsssssrsrs:sssssssss<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COGEMA<br />

08/14/87<br />

l<br />

1<br />

1<br />

l<br />

1<br />

1<br />

1<br />

1<br />

i<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

COB04AUG.WRI<br />

TOTAL t OF<br />

NUMBER OF GRAINS<br />

CAMPIE om f t-u t ir 1 i<br />

J*AMMFft ————— —————— -s———— *—— c KAR AQQAV<br />

BOB-87<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

123-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

124-01<br />

-02<br />

-03<br />

-M<br />

PANNING<br />

rniiiiiiiUv)<br />

Ifi<br />

iv<br />

—— - "- - . - - . . ..-- ————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

HlHjXCU —---———- —-——-—— ———-—— "—— *- rrw HOOHT<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

N 100 X 100 20 C 1 1<br />

1 35.2 43<br />

Y 50 X 125 18 C 1 1 EST. 2Z PYRITE<br />

75 X 75 15 C 1 1<br />

900 X 1200 110 C 1 1<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

3 43.0 21239<br />

Y 25 X 75 10 C 1 1 EST. li PYRITE<br />

50 X 50 10 C 2 2<br />

125 X 125 25 C 1 1<br />

125 X 175 29 C 1 1<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

W<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

W VISIBLE GOLD<br />

5 29.6 284


l l l<br />

l<br />

l l l<br />

l l<br />

l l<br />

l l<br />

l l<br />

l<br />

l l<br />

l<br />

GOLD CLASSIFICATION<br />

VISIBLE 60LD FROM SHAKING TABLE AND PANNING<br />

COGEMA 06/14/87<br />

COB04AUG.WRI<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNIN6S 10 ——————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

SAMPLE l PANNED rrrrrsrz ^-^- r^rz: srrsz HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-05 N NO VISIBLE GOLD<br />

124-06 N NO VISIBLE GOLD


1<br />

PAGE l COGEMA.' 06/18/87<br />

w<br />

1<br />

GOLD aASSIFICATION<br />

1 1111111<br />

1 1111111<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

t\ B-B B HHMP*-<br />

COB05AU6. HR1<br />

NUMBER OF GRAINS<br />

TOTAL 1 Cf PANN INGS 3 '————.———— , . . . -——— .<br />

ABRADED IRREGULAR DELICATE TOTAL WON CALC V.G.<br />

SAMPLE f PANNE<br />

: ^^,^ —— SSBBSS ssr ————-.—-.— — sss —————— sss flflG UAn ASSAY APPAV<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB<br />

BOB-87<br />

124-07<br />

N<br />

NO VISIBLE GOLD<br />

-08<br />

N<br />

NO VISIBLE GOLD<br />

-09<br />

N<br />

NO VISIBLE GOLD<br />

-10<br />

N<br />

NO VISIBLE GOLD<br />

-11<br />

N<br />

NO VISIBLE GOLD<br />

-12<br />

N<br />

50 X 75 13 C 1<br />

1<br />

1 28.7 13<br />

-13<br />

N<br />

NO VISIBLE GOLD<br />

-14<br />

N<br />

NO VISIBLE GOLD<br />

-15<br />

N<br />

NO VISIBLE GOLD<br />

-16<br />

N<br />

250 X 300 50 C 1<br />

1<br />

1 31.1 915<br />

125-01<br />

Y<br />

25 X 50 8 C<br />

75 X 100 18 C 1<br />

325 X 500 70 C 1<br />

1 1<br />

1<br />

1<br />

EST. IX PYRITE<br />

3 33.0 2725<br />

125A-01<br />

N<br />

NO VISIBLE GOLD<br />

-02<br />

N<br />

125 X 250 36 C 1<br />

1<br />

1 21.0 450<br />

-03<br />

N<br />

50 X 150 20 C 1<br />

1<br />

1 19.8 76<br />

126-01<br />

N<br />

100 X 125 22 C 1<br />

1<br />

1 32.5 65<br />

-02<br />

N<br />

NO VISIBLE GOLD<br />

-03<br />

N<br />

50 X 50 10 C 1<br />

1


PWQE2<br />

COBEHA<br />

08/18/87<br />

1 111111111111111111<br />

GOLD CLASSIFICATION<br />

— -srrrssrsr ——— s — z<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB05AUG.WRI<br />

TOTAL It OF PANNI<br />

CAMP) F t<br />

CTM R UC w<br />

BOB-87<br />

PANNFD<br />

y/N<br />

r nJVluU<br />

NUMBER OF GRAINS<br />

PvJO w --- — -.-— -— .--<br />

kjOr 7 ^,.^rrm..r m -.^. *-------.-. ~-.-.-<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

•^•— ——•— HWMV^HK W—MHM •.••^H MAf* ACCAV<br />

DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

1 18.1 H<br />

-04 N<br />

150 X 150 29 C 1 1<br />

1 38.0 130<br />

-05 N<br />

127-01 N<br />

-02 N<br />

-03 N<br />

-04 N<br />

-05 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

75 X 100 18 C 1 1<br />

1 42.0 24<br />

-06 N<br />

75 X 75 15 C 1 1<br />

1 31.0 21<br />

-07 N<br />

-08 N<br />

-09 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

150 X 200 34 C 1 1<br />

1 30.7 252<br />

-10 N<br />

-11 N<br />

NO VISIBLE GOLD<br />

50 X 50 10 C 1 1<br />

1 33.9 6<br />

-12 N<br />

-13 N<br />

-14 N<br />

-15 N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

PAGE 3 , t. COGEMA<br />

GOLD aASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB05AU6.WRI<br />

TOTAL l OF PANNINGS<br />

SAMPLE l<br />

PANNED<br />

Y/N DIAMETER THICKNESS<br />

BOB-87<br />

-16 50 X 75<br />

50 X 100<br />

75 X 75<br />

75 X 100<br />

100 X 125<br />

-17<br />

-18<br />

-19<br />

-20<br />

128-01<br />

N<br />

N<br />

O<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

50 X 75<br />

25 X 75<br />

50 X 75<br />

125 X 200<br />

175 X 250<br />

13 C<br />

15 C<br />

15 C<br />

18 C<br />

22C<br />

N 100 X 150 25 C<br />

NUMBER OF GRAINS<br />

"•""•"•*^~~"~*"""*"'*"~**"'*~~~~*'1*''~ i~"<br />

ABRADED IRREGULAR DELICATE TOTAL NON<br />

13 C l<br />

10 C<br />

13 C<br />

31 C<br />

40 C<br />

T<br />

GMS<br />

7 23.7<br />

l 30.9<br />

l 28.5<br />

l<br />

l<br />

l<br />

l<br />

CALC V.6.<br />

ASSAY<br />

PPB REMARKS<br />

206<br />

94<br />

13<br />

643<br />

EST. 21 PYRITE<br />

EST. 107. PYRITE<br />

08/18/87


1 111111111111111111<br />

PftGE i<br />

t<br />

BOLD CLASSIFICATION<br />

COGEMA<br />

08/19/87<br />

VISIBLE GOLD<br />

FROM SHAKING TABLE AND PANNING<br />

COBQ6AUG.WRI<br />

TOTAL 1 OF PANNI<br />

CAMP1 OHn.Lt P fc n<br />

PAKIKirh rnlxrttU<br />

Y/N<br />

*l"*r<br />

c<br />

ABRADED<br />

NUMBER OF GRAINS<br />

IRREGULAR DELICATE TOTAL m CALC V.G.<br />

srssrrrs rrrrrssrs rsr-s-r- —— c- MAR<br />

AQQAV<br />

DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-67<br />

128-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

-08<br />

-09<br />

-10<br />

-11<br />

-12<br />

-13<br />

-14<br />

-15<br />

-16<br />

129-01<br />

-02<br />

N<br />

N<br />

Y<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

N<br />

50 X 100 15 C 1 1<br />

NO VISIBLE GOLD<br />

1 25.8 25<br />

50 X 75 13 C 1 1 EST. IX PYRITE<br />

50 X 100 15 C 1 1<br />

50 X 125 18 C 1 1<br />

50 X 150 20 C 1 . 1<br />

100 X 150 25 C 1 1<br />

NO VISIBLE GOLD<br />

NO VISIBLE BOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

150 X 200 34 C 1 1<br />

NO VISIBLE SOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

75 X 100 18 C 1 1<br />

NO VISIBLE GOLD<br />

75 X 125 20 C 1 1<br />

5 .32.2 199<br />

1 27.3 283<br />

1 34.3 29<br />

1 27.8 54


l<br />

i l<br />

l l<br />

l<br />

PftGE. 2 C08EMA 08/19/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROM SHAKING TABLE AND PANNING<br />

COB06AUS.WRI<br />

NUMBER OF GRAINS<br />

TOTAL II OF PANNINGS 5 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.6.<br />

SMFLE l PANNED srsrsssr ^---- -—^-- sssss HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PPB (SHARKS<br />

BOB-87<br />

-03 N NO VISIBLE GOLD<br />

-04 N 175 X 275 42 C l i<br />

M l 23.9 670<br />

-05 N NO VISIBLE GOLD<br />

j| -06 N NO VISIBLE GOLD<br />

l'• -08 N 100 X 150 25 C l<br />

tm -07 N NO VISIBLE GOLD<br />

l 19.0 152<br />

l<br />

l<br />

i<br />

l<br />

l<br />

l<br />

l<br />

i<br />

i<br />

-09 N NO VISIBLE GOLD<br />

-10 Y 50 X 50 10 C 2 2 EST. 3Z PYRITE<br />

50 X 75 13 C l l<br />

75 l 125 20 C l l<br />

100 X 150 25 C l l<br />

125 X 150 27 C l l<br />

130-01 N 175 X 275 42 C l l<br />

-02 N NO VISIBLE GOLD<br />

-03 N NO VISIBLE GOLD<br />

-04 N NO VISIBLE GOLD<br />

-05 N NO VISIBLE GOLD<br />

-06 N 50 X 75 13 C l l<br />

-07 N NO VISIBLE GOLD<br />

-08 N NO VISIBLE GOLD<br />

6 15.6 575<br />

l 36.8 435<br />

l 18.2 20


1 111<br />

PA6E3<br />

COGEMA<br />

08/19/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD<br />

FROM SHAKING TABLE AND PAWING<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

COB06AUG.WRI<br />

NUMBER OF GRAINS<br />

TOTAL i OF PANNING3 5 ————————-————————<br />

ABRADED IRREGULAR DELICATE TOTAL NON CALC V.G.<br />

OMIITLC It rtWfK.ll ———— ' —— —— ' ————— — —— —— - ~ nno flJJMI<br />

Y/N DIAMETER THICKNESS T P T P T P CMS PPB REMARKS<br />

BOB-87<br />

-09<br />

-10<br />

131-01<br />

-02<br />

-03<br />

-04<br />

-05<br />

-06<br />

-07<br />

132-01<br />

-02<br />

-03<br />

-04<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

Y 25 X 75 10 C 1 1 EST. li PYRITE<br />

75 X 100 18 C 1 1<br />

100 X 125 22 C 1 1<br />

150 X 250 38 C 1 1<br />

N 25 X 50 8 C 1 1<br />

4 28.3 520<br />

1 31.5 3<br />

Y 75 X 75 15 C 1 1 EST. 2'/. PYRITE<br />

75 X 125 20 C 1 1<br />

N 50 X 75 13 C 1 1<br />

N<br />

N<br />

N<br />

N<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

NO VISIBLE GOLD<br />

N 100 X 200 29 C 1 1<br />

2 28.3 76<br />

1 24.0 16<br />

1 23.7 208<br />

Y 25 X 25 5 C 1 EST. T/. PYRITE<br />

25 X 50 8 C 1<br />

25 X 100 13 C 1<br />

50 X 75 13 C 1<br />

75 X 125 20 C 1<br />

100 X 125 22 C 1<br />

N 150 X 300 42 C 1 1<br />

6 23.6 190


l l<br />

i i i<br />

l<br />

i<br />

i<br />

i i i i<br />

i<br />

i i i<br />

i<br />

i i<br />

PW3E. A COGEMA 06/19/87<br />

GOLD CLASSIFICATION<br />

VISIBLE GOLD FROH SHAKING TABLE AND PAWING<br />

COBQ6AUG.WRI<br />

NUMBER OF GRAINS<br />

TOTAL l OF PANNINGS 5 ———————————————————<br />

ABRADED IRREGULAR DELICATE TOTAL WON CALC V.G.<br />

SAMPLE tt PANNED ssrssrrr ^~^ zrcrrszz ssrss HAG ASSAY<br />

Y/N DIAMETER THICKNESS T P T P T P 6MS PPB REMARKS<br />

BOB-87<br />

-05 N 350 X 375 63 C l l<br />

-06 N NO VISIBLE GOLD<br />

-07 N NO VISIBLE BOLD<br />

133-01 N 50 X 75 13 C l l<br />

i 24.9 643<br />

l 23.8 2608<br />

i 3K8 12


l l<br />

l<br />

l<br />

l l<br />

l<br />

A P P E N D I X III<br />

CHIMITEC HMC SAMPLE TREATMENT AND RESULTS<br />

- Treatment of Heavy Mineral Concentrate Samples<br />

I<br />

l<br />

- Listing of Chemistry Results<br />

- Listing of Second Analyses Results for Selected<br />

HMC Samples<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Ref. No. 87-CND-47-04<br />

Compiled by: J. Learn<br />

g (Doc. //0076U) January 1988<br />

l<br />

l


l l l<br />

l<br />

M<br />

TREATMENT OF HEAVY MINERAL CONCENTRATE SAMPLES<br />

Heavy mineral concentrate samples sent to Chimitec Ltee are treated in<br />

the following manner:<br />

1<br />

1. The entire sample is pulverized by hand in a ceramic plate<br />

to -150 mesh (105y).<br />

2. The entire sample is put in a capsule and analyzed by neutron<br />

1 activation for Au + 33 elements.<br />

l 3. Cu analyses are done by atomic absorption.<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

fiecor Hole Saep<br />

1 l<br />

2 l<br />

3 l<br />

4 l<br />

5 l<br />

6 l<br />

7 l<br />

8 l<br />

9 l<br />

l<br />

10<br />

11 2<br />

12 2<br />

13<br />

14<br />

2<br />

2<br />

15 2<br />

16 2<br />

17 2<br />

IB 2<br />

19 2<br />

20 2<br />

21<br />

22<br />

30<br />

31<br />

32<br />

33<br />

34<br />

2<br />

3<br />

23 3<br />

24 3<br />

25 3<br />

26 3<br />

27 3<br />

28 3<br />

29 3<br />

35 5<br />

36 5<br />

37 5<br />

38 5<br />

39 5<br />

40 5<br />

41 5<br />

42 6<br />

43 6<br />

44 6<br />

45 7<br />

46 7<br />

47 7<br />

48 7<br />

49 7<br />

50 7<br />

51 7<br />

52 7<br />

53 8<br />

54 8<br />

55 8<br />

RNTBUSH OVERBURDEN DRILLING<br />

>>> H<br />

ip<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

6<br />

9<br />

10<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

11<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

Au<br />

23500.0<br />

703.0<br />

14.0<br />

130.0<br />

200.0<br />

120.0<br />

17.0<br />

120.0<br />

75.0<br />

4.0<br />

120.0<br />

120.0<br />

120.0<br />

110.0<br />

207.0<br />

190.0<br />

24.0<br />

68.0<br />

1090.0<br />

293.0<br />

5.0<br />

209.0<br />

249.0<br />

228.0<br />

272.0<br />

-6.0<br />

21.0<br />

10.0<br />

-2.0<br />

56.0<br />

-6.0<br />

1600.0<br />

263.0<br />

3.0<br />

120.0<br />

13.0<br />

16.0<br />

61.0<br />

94.0<br />

64.0<br />

-2.0<br />

29.0<br />

7410.0<br />

-2.0<br />

235.0<br />

110.0<br />

57.0<br />

713.0<br />

1850.0<br />

24.0<br />

160.0<br />

-2.0<br />

-6.0<br />

26.0<br />

6.0<br />

Cu<br />

17.0<br />

22.0<br />

78.0<br />

60.0<br />

224.0<br />

106.0<br />

114.0<br />

196.0<br />

136.0<br />

51.0<br />

64.0<br />

141.0<br />

158.0<br />

192.0<br />

90.0<br />

142.0<br />

186.0<br />

150.0<br />

201.0<br />

170.0<br />

53.0<br />

26.0<br />

18.0<br />

38.0<br />

222.0<br />

124.0<br />

283.0<br />

144.0<br />

45.0<br />

242.0<br />

160.0<br />

178.0<br />

108.0<br />

32.0<br />

256.0<br />

174.0<br />

148.0<br />

178.0<br />

193.0<br />

114.0<br />

47.0<br />

376.0<br />

254.0<br />

46.0<br />

18.0<br />

16.0<br />

130.0<br />

155.0<br />

222.0<br />

596.0<br />

294.0<br />

42.0<br />

124.0<br />

242.0<br />

50.0<br />

As<br />

2.0<br />

3.9<br />

22.0<br />

16.0<br />

78.0<br />

98.6<br />

57.6<br />

68.5<br />

73.4<br />

10.0<br />

7.0<br />

28.0<br />

33.0<br />

34.0<br />

16.0<br />

38.0<br />

91.6<br />

196.0<br />

49.0<br />

54.8<br />

1.2<br />

3.8<br />

2.8<br />

2.9<br />

25.0<br />

27.0<br />

19.0<br />

18.0<br />

0.7<br />

90.1<br />

28.0<br />

37.0<br />

23.0<br />

1.3<br />

37.0<br />

41.0<br />

21.0<br />

29.0<br />

38.0<br />

37.0<br />

-0.5<br />

59.8<br />

68.2<br />

-0.5<br />

2.5<br />

1.9<br />

16.0<br />

19.0<br />

31.0<br />

54.0<br />

47.0<br />

-0.5<br />

14.0<br />

16.0<br />

0.6<br />

Sb<br />

0.3<br />

0.4<br />

0.6<br />

0.4<br />

0.6<br />

1.4<br />

0.9<br />

0.8<br />

1.2<br />

0.1<br />

0.4<br />

0.4<br />

0.5<br />

0.4<br />

0.5<br />

0.4<br />

1.1<br />

3.1<br />

1.0<br />

1.6<br />

-0.1<br />

0.4<br />

0.4<br />

0.3<br />

0.5<br />

0.4<br />

0.7<br />

0.8<br />

0.1<br />

0.9<br />

0.5<br />

0.5<br />

0.6<br />

-O.I<br />

0.6<br />

0.6<br />

0.6<br />

0.6<br />

0.6<br />

0.4<br />

-0.1<br />

0.8<br />

1.0<br />

-0.1<br />

0.3<br />

0.2<br />

0.4<br />

0.3<br />

0.6<br />

0.8<br />

4.7<br />

-0.1<br />

0.4<br />

0.5<br />

-0.1<br />

Ba<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

110.0<br />

-50.0<br />

660.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

82.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

560.0<br />

93.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

93.0<br />

750.0<br />

- -50.0<br />

. -50.0<br />

-50.0<br />

-50.0<br />

: 750.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

83.0<br />

-50.0<br />

740.0<br />

-50.0<br />

-50.0<br />

740.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

620.0<br />

-50.0<br />

-50.0<br />

630.0<br />

Cd<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

6.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

9.0<br />

7.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

12.0<br />

14.0<br />

-10.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

12.0<br />

6.0<br />

-5.0<br />

-5.0<br />

7.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

13.0<br />

-5.0<br />

-5.0<br />

7.0<br />

-5.0<br />

Cs<br />

-0.5<br />

-0.5<br />

0.7<br />

1.1<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

5.4<br />

-0.5<br />

-0.5<br />

-0.5<br />

0.6<br />

-0.5<br />

-0.5<br />

0.7<br />

-0.5<br />

-0.5<br />

1.1<br />

3.5<br />

0.8<br />

0.7<br />

•-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.1<br />

7.1<br />

-0.5<br />

i.O<br />

-0.5<br />

-0.5<br />

4.3<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

0.9<br />

-0.5<br />

6.7<br />

-0.5<br />

0.5<br />

4.7<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

5.6<br />

-0.5<br />

-0.5<br />

3.9<br />

M<br />

C<br />

Cr<br />

480.0<br />

550.0<br />

570.0<br />

590.0<br />

480.0<br />

530.0<br />

570.0<br />

610.0<br />

480.0<br />

280.0<br />

550.0<br />

510.0<br />

540.0<br />

550.0<br />

460.0<br />

540.0<br />

570.0<br />

560.0<br />

600.0<br />

620.0<br />

310.0<br />

580.0<br />

630.0<br />

620.0<br />

590.0<br />

490.0<br />

490.0<br />

510.0<br />

320.0<br />

540.0<br />

500.0<br />

570.0<br />

540.0<br />

340.0<br />

650.0<br />

580.0<br />

540.0<br />

510.0<br />

530.0<br />

550.0<br />

310.0<br />

400.0<br />

340.0<br />

460.0<br />

520.0<br />

570.0<br />

550.0<br />

480.0<br />

530.0<br />

370.0<br />

430.0<br />

290.0<br />

500.0<br />

460.0<br />

280.0<br />

•(*X [87/12/22]<br />

Co<br />

26.0<br />

36.0<br />

97.0<br />

80.0<br />

200.0<br />

150.0<br />

120.0<br />

170.0<br />

120.0<br />

26.0<br />

75.0<br />

140.0<br />

150.0<br />

160.0<br />

93.0<br />

150.0<br />

140.0<br />

160.0<br />

130.0<br />

150.0<br />

26.0<br />

41.0<br />

34.0<br />

39.0<br />

190.0<br />

130.0<br />

240.0<br />

150.0<br />

25.0<br />

220.0<br />

200.0<br />

240.0<br />

150.0<br />

29.0<br />

180.0<br />

190.0<br />

140.0<br />

200.0<br />

190.0<br />

120.0<br />

32.0<br />

290.0<br />

280.0<br />

33.0<br />

38.0<br />

34.0<br />

120.0<br />

140.0<br />

220.0<br />

330.0<br />

240.0<br />

27.0<br />

99.0<br />

150.0<br />

32.0<br />

Eu<br />

6.0<br />

6.0<br />

7.0<br />

8.0<br />

6.0<br />

6.0<br />

6.0<br />

6.0<br />

7.0<br />

-1.0<br />

7.0<br />

6.0<br />

7.0<br />

7.0<br />

8.0<br />

7.0<br />

5.0<br />

5.0<br />

7.0<br />

8.0<br />

2.0<br />

6.0<br />

6.0<br />

8.0<br />

8.0<br />

6.0<br />

5.0<br />

7.0<br />

1.0<br />

5.0<br />

5.0<br />

6.0<br />

6.0<br />

-1.0<br />

5.0<br />

6.0<br />

6.0<br />

7.0<br />

6.0<br />

6.0<br />

2.0<br />

5.0<br />

5.0<br />

1.0<br />

7.0<br />

6.0<br />

7.0<br />

5,0<br />

6.0<br />

4.0<br />

6.0<br />

1.0<br />

7.0<br />

6.0<br />

-1.0<br />

Hf<br />

229.0<br />

246.0<br />

268.0<br />

243.0<br />

185.0<br />

192.0<br />

213.0<br />

249.0<br />

190.0<br />

4.0<br />

267.0<br />

245.0<br />

246.0<br />

245.0<br />

231.0<br />

229.0<br />

202.0<br />

209.0<br />

222.0<br />

243.0<br />

4.0<br />

308.0<br />

326.0<br />

321.0<br />

290.0<br />

241.0<br />

228.0<br />

261.0<br />

3.0<br />

162.0<br />

227.0<br />

205.0<br />

228.0<br />

4.0<br />

167.0<br />

209.0<br />

256.0<br />

191.0<br />

181.0<br />

255.0<br />

4.0<br />

79.0<br />

66.0<br />

5.0<br />

315.0<br />

345.0<br />

296.0<br />

256.0<br />

252.0<br />

61.0<br />

152.0<br />

4.0<br />

242.0<br />

189.0<br />

4.0<br />

Ir<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Saep<br />

56<br />

57<br />

58<br />

59<br />

60<br />

61 9<br />

62 9<br />

63<br />

64<br />

65<br />

66<br />

67 10<br />

68 10<br />

69 10<br />

70 10<br />

71 10<br />

72 11<br />

73 11<br />

74 12<br />

75 12<br />

76 12<br />

77 12<br />

78 12<br />

79 12<br />

80 12<br />

81 12<br />

62 12<br />

83 12<br />

84 12<br />

85 12<br />

86 12<br />

87 12<br />

88 12<br />

89 12<br />

90 12<br />

91 12<br />

92 12<br />

93 12<br />

94 13<br />

95 13<br />

96 13<br />

97 13<br />

98 14<br />

99 14<br />

100 14<br />

101 15<br />

102 15<br />

103 16<br />

104 16<br />

105 16<br />

106 16<br />

107 16<br />

108 16<br />

109 16<br />

110 17<br />

111 17<br />

RNTBUSH OVERBURDEN DRILLING<br />

>>> H<br />

lep<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

11<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

Au<br />

-5.0<br />

93.0<br />

110.0<br />

60.0<br />

94.0<br />

21.0<br />

223.0<br />

18.0<br />

54.0<br />

54.0<br />

6.0<br />

130.0<br />

24.0<br />

485.0<br />

160.0<br />

-2.0<br />

47.0<br />

3.0<br />

1270.0<br />

352.0<br />

130.0<br />

55.0<br />

140.0<br />

110.0<br />

130.0<br />

30.0<br />

1490.0<br />

337.0<br />

33.0<br />

6020.0<br />

1300.0<br />

439.0<br />

373.0<br />

868.0<br />

764.0<br />

413.0<br />

-13.0<br />

3.0<br />

1320.0<br />

52.0<br />

97.0<br />

-2.0<br />

243.0<br />

-9.0<br />

6.0<br />

48.0<br />

-2.0<br />

71.0<br />

130.0<br />

249.0<br />

31.0<br />

160.0<br />

607.0<br />

4.0<br />

1100.0<br />

2350.0<br />

Cu<br />

172.0<br />

126.0<br />

114.0<br />

176.0<br />

128.0<br />

128.0<br />

216.0<br />

148.0<br />

216.0<br />

158.0<br />

47.0<br />

182.0<br />

142.0<br />

176.0<br />

236.0<br />

54.0<br />

148.0<br />

48.0<br />

202.0<br />

142.0<br />

154.0<br />

86.0<br />

108.0<br />

128.0<br />

92.0<br />

192.0<br />

64.0<br />

98.0<br />

82.0<br />

102.0<br />

53.0<br />

24.0<br />

14.0<br />

42.0<br />

50.0<br />

28.0<br />

38.0<br />

48.0<br />

182.0<br />

132.0<br />

152.0<br />

43.0<br />

146.0<br />

190.0<br />

40.0<br />

245.0<br />

52.0<br />

130.0<br />

100.0<br />

66.0<br />

130.0<br />

194.0<br />

178.0<br />

35.0<br />

14.0<br />

18.0<br />

As<br />

24.0<br />

19.0<br />

18.0<br />

21.0<br />

36.0<br />

25.0<br />

34.0<br />

20.0<br />

29.0<br />

19.0<br />

0.9<br />

67.7<br />

87.2<br />

24.0<br />

25.0<br />

1.2<br />

28.0<br />

0.6<br />

28.0<br />

24.0<br />

28.0<br />

18.0<br />

29.0<br />

19.0<br />

23.0<br />

30.0<br />

69.4<br />

47.0<br />

20.0<br />

32.0<br />

5.3<br />

-4.1<br />

-4.5<br />

-3.9<br />

7.0<br />

-3.2<br />

6.8<br />

-0.5<br />

7.3<br />

71.6<br />

39.0<br />

0.6<br />

33.0<br />

34.0<br />

0.6<br />

28.0<br />

-0.5<br />

17.0<br />

16.0<br />

22.0<br />

21.0<br />

52.2<br />

20.0<br />

-0.5<br />

-3.5<br />

3.7<br />

Sb<br />

0.4<br />

0.4<br />

0.4<br />

0.6<br />

0.6<br />

0.5<br />

0.4<br />

0.3<br />

0.4<br />

0.5<br />

0.1<br />

0.6<br />

0.6<br />

0.4<br />

0.6<br />

0.2<br />

0.4<br />

-0.1<br />

0.5<br />

0.5<br />

0.3<br />

0.4<br />

0.5<br />

0.4<br />

0.5<br />

0.3<br />

0.5<br />

0.4<br />

0.3<br />

-0.8<br />

0.3<br />

-0.3<br />

1.7<br />

1.7<br />

0.4<br />

-0.1<br />

-0.2<br />

-0.1<br />

0.4<br />

0.6<br />

0.4<br />

-0.1<br />

0.5<br />

0.6<br />

-0.1<br />

0.5<br />

0.1<br />

0.4<br />

0.6<br />

0.6<br />

0.4<br />

0.7<br />

0.9<br />

-0.1<br />

0.3<br />

0.4<br />

Ba<br />

83.0<br />

-50.0<br />

-50.0<br />

110.0<br />

-50.0<br />

-50.0<br />

78.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

500.0<br />

-50.0<br />

-110.0<br />

-50.0<br />

-50.0<br />

610.0<br />

-50.0<br />

720.0<br />

-50.0<br />

120.0<br />

120.0<br />

-50.0<br />

-50.0<br />

-100.0<br />

190.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-110.0<br />

-110.0<br />

-120.0<br />

-150.0<br />

-120.0<br />

-120.0<br />

-50.0<br />

-140.0<br />

520.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

710.0<br />

-50.0<br />

160.0<br />

650.0<br />

-50.0<br />

960.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

180.0<br />

590.0<br />

-50.0<br />

-50.0<br />

Cd<br />

7.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5,0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-15.0<br />

-13.0<br />

-13.0<br />

-5.0<br />

-13.0<br />

-5.0<br />

-12.0<br />

-11.0<br />

-11.0<br />

-11.0<br />

-13.0<br />

- -14.0<br />

-13.0<br />

-10.0<br />

-13.0<br />

-12.0<br />

-10.0<br />

-16.0<br />

-16.0<br />

-18.0<br />

-20.0<br />

-17.0<br />

-17.0<br />

17.0<br />

-19.0<br />

-5.0<br />

-14.0<br />

-15.0<br />

-15.0<br />

-5.0<br />

-14.0<br />

-13.0<br />

-5.0<br />

-13.0<br />

-5.0<br />

-12.0<br />

-13.0<br />

-13.0<br />

-15.0<br />

-12.0<br />

-14.0<br />

-5.0<br />

-15.0<br />

-12.0<br />

Cs<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

0.9<br />

-0.5<br />

2.0<br />

-0.5<br />

-1.2<br />

-0.5<br />

-1.0<br />

2.5<br />

-0.5<br />

5.1<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.3<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-1.2<br />

-1.2<br />

-1.4<br />

2.1<br />

-1.3<br />

-1.3<br />

-1.0<br />

-1.5<br />

1.4<br />

1.4<br />

1.5<br />

-l.l<br />

4.2<br />

-1.0<br />

-0.5<br />

4.7<br />

-0.5<br />

6.2<br />

-0.5<br />

1.1<br />

-0.5,<br />

-1.1<br />

-0.5<br />

-0.5<br />

4.2<br />

-1.1<br />

-0.5<br />

M<br />

C<br />

Cr<br />

550.0<br />

560.0<br />

490.0<br />

510.0<br />

500.0<br />

520.0<br />

540.0<br />

570.0<br />

570,0<br />

470.0<br />

280.0<br />

580.0<br />

560.0<br />

610.0<br />

690.0<br />

350,0<br />

600.0<br />

290.0<br />

590.0<br />

610.0<br />

550,0<br />

650.0<br />

660.0<br />

700.0<br />

600.0<br />

540.0<br />

640.0<br />

640.0<br />

510.0<br />

570.0<br />

600.0<br />

610.0<br />

870.0<br />

710.0<br />

540.0<br />

730.0<br />

770.0<br />

210.0<br />

600.0<br />

690.0<br />

580.0<br />

330.0<br />

650.0<br />

600.0<br />

310.0<br />

600.0<br />

310,0<br />

580.0<br />

550.0<br />

660.0<br />

660.0<br />

580.0<br />

620.0<br />

170.0<br />

630.0<br />

690.0<br />


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Satp<br />

112 17<br />

113 17<br />

114 17<br />

115 17<br />

116 17<br />

117 17<br />

118 17<br />

119 17<br />

120 17<br />

121 17<br />

122 17<br />

123 17<br />

124 17<br />

125 17<br />

126 17<br />

127 17<br />

128 17<br />

129 17<br />

130 17<br />

131 18<br />

132 18<br />

133 18<br />

134 18<br />

135 18<br />

136 18<br />

137 19<br />

138 19<br />

139 19<br />

140 19<br />

141 19<br />

142 19<br />

143 19<br />

144 20<br />

145 20<br />

146 20<br />

147 20<br />

148 20<br />

149 20<br />

150 20<br />

151 20<br />

152 20<br />

153 20<br />

154 20<br />

155 20<br />

156 20<br />

157 20<br />

158 20<br />

159 20<br />

160 21<br />

161 21<br />

162 21<br />

163 21<br />

164 21<br />

165 21<br />

166 21<br />

167 21<br />

RNTBUSH OVERBURDEN DRILLING >>> HMD


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

4 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

5 of BURNTBUSH OVERBURDEN DRILLING >>> HMD [87/12/223<br />

Recor Hole Sasp Au Cu As Sb Ba Cd Cs Cr Co Eu Hf Ir<br />

224<br />

225<br />

226<br />

227<br />

228<br />

229<br />

230<br />

231<br />

232<br />

233<br />

234<br />

235<br />

236<br />

237<br />

238<br />

239<br />

240<br />

241<br />

242<br />

243<br />

244<br />

245<br />

246<br />

247<br />

248<br />

249<br />

250<br />

251<br />

252<br />

253<br />

254<br />

255<br />

256<br />

257<br />

258<br />

259<br />

260<br />

261<br />

262<br />

263<br />

264<br />

265<br />

266<br />

267<br />

268<br />

269<br />

270<br />

271<br />

272<br />

273<br />

274<br />

275<br />

276<br />

277<br />

278<br />

279<br />

25<br />

25<br />

25<br />

25<br />

25<br />

25<br />

25<br />

25<br />

25<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

26<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

27<br />

28<br />

28<br />

28<br />

28<br />

28<br />

28<br />

28<br />

28<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

23<br />

24<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

e<br />

130.0<br />

36.0<br />

17.0<br />

93.0<br />

120.0<br />

-10.0<br />

37.0<br />

1910.0<br />

-2.0<br />

247.0<br />

673.0<br />

56.0<br />

-7.0<br />

190.0<br />

33.0<br />

73.0<br />

47.0<br />

46.0<br />

190.0<br />

99.0<br />

25.0<br />

34.0<br />

31.0<br />

150.0<br />

16.0<br />

234.0<br />

1190.0<br />

238.0<br />

802.0<br />

13.0<br />

150.0<br />

223.0<br />

-2.0<br />

74.0<br />

46.0<br />

31.0<br />

110.0<br />

328.0<br />

542.0<br />

37.0<br />

-9.0<br />

23.0<br />

16.0<br />

445.0<br />

21.0<br />

295.0<br />

130.0<br />

-2.0<br />

18.0<br />

514.0<br />

14.0<br />

110.0<br />

1730.0<br />

503.0<br />

226,0<br />

-2.0<br />

184.0<br />

224.0<br />

192.0<br />

154.0<br />

162.0<br />

210.0<br />

144.0<br />

170.0<br />

38.0<br />

14.0<br />

22.0<br />

228.0<br />

184.0<br />

28.0<br />

90.0<br />

100.0<br />

92.0<br />

102.0<br />

90.0<br />

92.0<br />

116.0<br />

92.0<br />

202.0<br />

152.0<br />

142.0<br />

218.0<br />

190.0<br />

230.0<br />

172.0<br />

276.0<br />

52.0<br />

16.0<br />

49.0<br />

144.0<br />

118.0<br />

130.0<br />

194.0<br />

212.0<br />

160.0<br />

238.0<br />

232.0<br />

118.0<br />

188.0<br />

150.0<br />

98.0<br />

84.0<br />

84.0<br />

43.0<br />

142.0<br />

64.0<br />

40.0<br />

46.0<br />

48.0<br />

320.0<br />

174.0<br />

50.0<br />

29.0<br />

23.0<br />

28.0<br />

25.0<br />

28.0<br />

33.0<br />

77.3<br />

47.0<br />

1.1<br />

-3.2<br />

12.0<br />

-3.4<br />

45.0<br />

4.0<br />

19.0<br />

16.0<br />

23.0<br />

17.0<br />

22.0<br />

35.0<br />

46.0<br />

20.0<br />

31.0<br />

25.0<br />

20.0<br />

31.0<br />

20.0<br />

34.0<br />

17.0<br />

18.0<br />

7.5<br />

-2.8<br />

-0.5<br />

19.0<br />

15.0<br />

28.0<br />

45.0<br />

33.0<br />

26.0<br />

37.0<br />

30.0<br />

54.3<br />

37.0<br />

38.0<br />

28.0<br />

25.0<br />

25.0<br />

-0.5<br />

28.0<br />

21.0<br />

15.0<br />

18.0<br />

11.0<br />

32.0<br />

16,0<br />

-0.5<br />

0.7<br />

0.3<br />

0.4<br />

0.5<br />

0.7<br />

0.9<br />

0.8<br />

0.6<br />

-0.1<br />

0.3<br />

0.3<br />

0.6<br />

0.5<br />

0.3<br />

0.4<br />

0.5<br />

0.4<br />

0.8<br />

0.6<br />

0.4<br />

0.7<br />

0.4<br />

0.5<br />

0.3<br />

0.5<br />

0.7<br />

0.5<br />

1.0<br />

0.4<br />

0.5<br />

0.5<br />

0.4<br />

-0.1<br />

0.5<br />

0.5<br />

0.3<br />

0.6<br />

0.5<br />

0.4<br />

1.0<br />

0.7<br />

0.7<br />

0.6<br />

0.6<br />

0.4<br />

0.4<br />

0.5<br />

-0.1<br />

0.6<br />

0.6<br />

0.4<br />

0.4<br />

0.4<br />

0.3<br />

0.3<br />

-0.1<br />

-50.0<br />

-50.0<br />

-50.0<br />

210.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

1100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

140.0<br />

130.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

240.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

140.0<br />

-100.0<br />

730.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-110.0<br />

-50.0<br />

160.0<br />

-50.0<br />

-110.0<br />

-110.0<br />

-120.0<br />

-110.0<br />

750.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

890.0<br />

-12.0<br />

-12.0<br />

-13.0<br />

24.0<br />

-13.0<br />

-12.0<br />

-12.0<br />

-15.0<br />

-5.0<br />

-12.0<br />

-13.0<br />

-13.0<br />

-11.0<br />

-12.0<br />

-11,0<br />

-10.0<br />

-12.0<br />

-11.0<br />

-11.0<br />

-20.0<br />

16.0<br />

-13.0<br />

-12.0<br />

-12.0<br />

-13.0<br />

-12.0<br />

-13.0<br />

-11.0<br />

-11.0<br />

-12.0<br />

-12.0<br />

-14.0<br />

-5.0<br />

-13.0<br />

-12.0<br />

-13.0<br />

-12.0<br />

-12.0<br />

-11.0<br />

-15.0<br />

-12.0<br />

-13.0<br />

-12.0<br />

-15.0<br />

-16.0<br />

-16.0<br />

-16.0<br />

-5.0<br />

-12.0<br />

-12.0<br />

-11.0<br />

-14.0<br />

-14.0<br />

-13.0<br />

-11.0<br />

-5.0<br />

0.8<br />

-0.5<br />

-0.5<br />

-1.0<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

19.0<br />

-0.5<br />

1.7<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.0<br />

-0.5<br />

-0.5<br />

1.7<br />

-0.5<br />

-1.0<br />

-0.5<br />

-0.5<br />

-1.1<br />

-0.5<br />

-1.1<br />

-0.5<br />

1.5<br />

-0.5<br />

-0.5<br />

-1.1<br />

5.1<br />

-1.0<br />

-0.5<br />

-1.0<br />

-0.5<br />

-0.5<br />

-0.5<br />

-1.3<br />

-0.5<br />

-1.0<br />

-0.5<br />

-1.2<br />

-1.2<br />

1.5<br />

-1.2<br />

7.6<br />

-0.5<br />

-0.5<br />

-0.5<br />

-1.1<br />

-1.1<br />

-0.5<br />

-0.5<br />

6.3<br />

820.0<br />

840.0<br />

990.0<br />

1200.0<br />

1000.0<br />

860.0<br />

860.0<br />

1100.0<br />

760.0<br />

700.0<br />

720.0<br />

620.0<br />

510.0<br />

610.0<br />

560.0<br />

610.0<br />

620.0<br />

630.0<br />

620.0<br />

980.0<br />

650.0<br />

1000.0<br />

900.0<br />

970.0<br />

1000.0<br />

980.0<br />

710.0<br />

870.0<br />

850.0<br />

960.0<br />

960.0<br />

970.0<br />

270.0<br />

630.0<br />

660.0<br />

990.0<br />

920.0<br />

990.0<br />

970.0<br />

1000.0<br />

940.0<br />

780.0<br />

950.0<br />

1000.0<br />

1200.0<br />

1100.0<br />

940.0<br />

300.0<br />

940.0<br />

1000.0<br />

930.0<br />

1100.0<br />

1200.0<br />

1100.0<br />

950,0<br />

280,0<br />

210.0<br />

210.0<br />

180.0<br />

170.0<br />

170.0<br />

160.0<br />

160.0<br />

220.0<br />

46.0<br />

39.0<br />

61.0<br />

160.0<br />

130.0<br />

53.0<br />

110.0<br />

110.0<br />

110.0<br />

100.0<br />

110.0<br />

180.0<br />

120.0<br />

88.0<br />

170.0<br />

140.0<br />

130.0<br />

220.0<br />

210.0<br />

230.0<br />

160.0<br />

170.0<br />

64.0<br />

28.0<br />

24.0<br />

150.0<br />

110.0<br />

120.0<br />

190.0<br />

160.0<br />

160.0<br />

230.0<br />

200.0<br />

210.0<br />

170.0<br />

160.0<br />

120.0<br />

120.0<br />

110.0<br />

32.0<br />

140.0<br />

110.0<br />

57.0<br />

63.0<br />

68.0<br />

90.0<br />

160.0<br />

33.0<br />

8.0<br />

6.0<br />

8.0<br />

8.0<br />

7.0<br />

7.0<br />

9.0<br />

13.0<br />

3.0<br />

9.0<br />

10.0<br />

12.0<br />

10.0<br />

8.0<br />

9.0<br />

6.0<br />

7.0<br />

6.0<br />

6.0<br />

12.0<br />

9.0<br />

4.0<br />

5.0<br />

5.0<br />

8.0<br />

7.0<br />

10.0<br />

5.0<br />

8.0<br />

7.0<br />

10.0<br />

11.0<br />

1.0<br />

5.0<br />

7.0<br />

6.0<br />

6.0<br />

6.0<br />

4.0<br />

5.0<br />

6.0<br />

6.0<br />

5.0<br />

6.0<br />

7.0<br />

4.0<br />

5.0<br />

1.0<br />

4.0<br />

5.0<br />

5.0<br />

5.0<br />

6.0<br />

4.0<br />

4.0<br />

2.0<br />

249.0<br />

291.0<br />

376.0<br />

325,0<br />

275.0<br />

220.0<br />

185.0<br />

140.0<br />

5.0<br />

341.0<br />

350.0<br />

336.0<br />

274.0<br />

333.0<br />

265.0<br />

269.0<br />

283.0<br />

294.0<br />

263.0<br />

526.0<br />

283.0<br />

243.0<br />

126.0<br />

167.0<br />

240.0<br />

185.0<br />

194.0<br />

182,0<br />

194.0<br />

151.0<br />

201.0<br />

175.0<br />

4.0<br />

273.0<br />

270.0<br />

331.0<br />

226.0<br />

205.0<br />

174.0<br />

203.0<br />

176.0<br />

205.0<br />

259.0<br />

344.0<br />

293.0<br />

361.0<br />

327.0<br />

5.0<br />

238.0<br />

239.0<br />

209.0<br />

249.0<br />

267.0<br />

256.0<br />

199.0<br />

3.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Saip<br />

280 29<br />

281 29<br />

282 29<br />

283 29<br />

284 29<br />

285 29<br />

286 29<br />

287 29<br />

288 29<br />

289 29<br />

290 29<br />

291 29<br />

292 29<br />

293 29<br />

294 29<br />

295 29<br />

296 30<br />

297 30<br />

298 30<br />

299 30<br />

300 30<br />

301 30<br />

302 30<br />

303 30<br />

304 30<br />

305 30<br />

306 30<br />

307 30<br />

308 30<br />

309 30<br />

310 30<br />

311 30<br />

312 30<br />

313 30<br />

314 30<br />

315 30<br />

316 30<br />

317 31<br />

318 31<br />

319 31<br />

320 31<br />

321 31<br />

322 31<br />

323 31<br />

324 31<br />

325 31<br />

326 31<br />

327 31<br />

328 31<br />

329 31<br />

330 31<br />

331 31<br />

332 31<br />

333 31<br />

334 31<br />

335 31<br />

RNTBUBH OVERBURDEN DRILLING<br />

>>> H<br />

*P<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

Au<br />

16.0<br />

-7.0<br />

14.0<br />

-9.0<br />

110.0<br />

14.0<br />

-10.0<br />

110.0<br />

89.0<br />

16.0<br />

47.0<br />

170.0<br />

53.0<br />

110,0<br />

89.0<br />

-2.0<br />

689.0<br />

100.0<br />

251.0<br />

460.0<br />

-9.0<br />

120.0<br />

30.0<br />

49.0<br />

73.0<br />

-9.0<br />

13.0<br />

100.0<br />

-8.0<br />

-11.0<br />

55.0<br />

28.0<br />

91.0<br />

120.0<br />

110.0<br />

77.0<br />

-2.0<br />

246.0<br />

68.0<br />

46.0<br />

150.0<br />

13.0<br />

190.0<br />

76.0<br />

95.0<br />

18.0<br />

6260.0<br />

-9.0<br />

83.0<br />

19.0<br />

65.0<br />

B53.0<br />

205.0<br />

42.0<br />

1680.0<br />

-8.0<br />

Cu<br />

120.0<br />

136.0<br />

149.0<br />

126.0<br />

122.0<br />

BO.O<br />

120.0<br />

172.0<br />

158.0<br />

108.0<br />

34.0<br />

132.0<br />

78.0<br />

38.0<br />

78.0<br />

72.0<br />

44.0<br />

90.0<br />

74.0<br />

114.0<br />

90.0<br />

86.0<br />

104.0<br />

114.0<br />

96.0<br />

102.0<br />

82.0<br />

110.0<br />

20.0<br />

114.0<br />

10.0<br />

4.0<br />

6.0<br />

8.0<br />

30.0<br />

373.0<br />

61.0<br />

20.0<br />

20.0<br />

10.0<br />

88.0<br />

72.0<br />

78.0<br />

100.0<br />

62.0<br />

112.0<br />

50.0<br />

264.0<br />

170.0<br />

160.0<br />

146.0<br />

208.0<br />

140.0<br />

110.0<br />

119.0<br />

100.0<br />

As<br />

8.3<br />

12.0<br />

19.0<br />

14.0<br />

23.0<br />

15.0<br />

24.0<br />

22.0<br />

25.0<br />

28.0<br />

19.0<br />

22.0<br />

20.0<br />

24.0<br />

36.0<br />

1.0<br />

10.0<br />

15.0<br />

18.0<br />

26.0<br />

38.0<br />

22.0<br />

19.0<br />

21.0<br />

27.0<br />

20.0<br />

20.0<br />

21.0<br />

21.0<br />

20.0<br />

3.3<br />

-3.4<br />

-3.0<br />

-2.8<br />

8.0<br />

23.0<br />

0.7<br />

-3.1<br />

-2.8<br />

-2.5<br />

2.4<br />

22.0<br />

10.0<br />

25.0<br />

7.4<br />

15.0<br />

34.0<br />

19.0<br />

20.0<br />

21.0<br />

11.0<br />

78.5<br />

30.0<br />

24.0<br />

31.0<br />

14.0<br />

Sb<br />

0.4<br />

0.4<br />

0.5<br />

0.5<br />

0.5<br />

0.4<br />

0.6<br />

0.6<br />

0.6<br />

0.5<br />

0.7<br />

0.6<br />

0.5<br />

0.4<br />

0.6<br />

0.1<br />

0.4<br />

0.5<br />

0.4<br />

0.5<br />

0.7<br />

0.5<br />

0.4<br />

0.4<br />

0.5<br />

0.5<br />

0.6<br />

0.5<br />

0.7<br />

0.4<br />

0.4<br />

0.3<br />

0.3<br />

0.3<br />

0.5<br />

0.4<br />

-0.1<br />

0.3<br />

0.5<br />

0.3<br />

0.3<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.7<br />

0.5<br />

0.4<br />

0.4<br />

0.4<br />

0.5<br />

0.4<br />

0.5<br />

0.5<br />

0.4<br />

Ba<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

450.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

140.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-110.0<br />

-110.0<br />

-110.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

740.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

Cd<br />

-12.0<br />

-11.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

14.0<br />

-14.0<br />

-13.0<br />

13.0<br />

-5.0<br />

-5.0<br />

-11.0<br />

-11.0<br />

-11.0<br />

-10.0<br />

-5.0<br />

-13.0<br />

-12.0<br />

-10.0<br />

-13.0<br />

-13.0<br />

-13.0<br />

-5.0<br />

-13.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

-13.0<br />

-12.0<br />

-16.0<br />

-14.0<br />

-16.0<br />

-14.0<br />

-13.0<br />

-12.0<br />

-12.0<br />

-5.0<br />

-15.0<br />

-13.0<br />

-12.0<br />

-10.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

-11.0<br />

-12.0<br />

-13.0<br />

-12.0<br />

-11.0<br />

12.0<br />

-12.0<br />

17.0<br />

-11.0<br />

-12.0<br />

-12.0<br />

Cs<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-1.0<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

2.8<br />

-1.1<br />

-0.5<br />

-0.5<br />

-1.1<br />

-0.5<br />

-1.0<br />

-0.5<br />

-1.0<br />

-0.5<br />

-0,5<br />

.6<br />

- .1<br />

- .5<br />

- .3<br />

.4<br />

- .2<br />

-1.1<br />

-1.0<br />

-0.5<br />

-0.5<br />

2.6<br />

-1.1<br />

-1.0<br />

-0.5<br />

-0.5<br />

1.1<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.1<br />

-0.5<br />

-0.5<br />

1.5<br />

-0.5<br />

M<br />

C<br />

Cr<br />

920.0<br />

870.0<br />

860.0<br />

910.0<br />

810.0<br />

710.0<br />

830.0<br />

790.0<br />

1000.0<br />

730.0<br />

800.0<br />

890.0<br />

950.0<br />

1000.0<br />

970.0<br />

390.0<br />

970.0<br />

910.0<br />

760.0<br />

1000.0<br />

940.0<br />

1000.0<br />

730.0<br />

1000.0<br />

960.0<br />

1000.0<br />

880.0<br />

1000.0<br />

790.0<br />

1100.0<br />

880.0<br />

1000.0<br />

1100.0<br />

900.0<br />

790.0<br />

740.0<br />

360.0<br />

1000.0<br />

950.0<br />

790.0<br />

750.0<br />

800.0<br />

810.0<br />

780.0<br />

840.0<br />

810.0<br />

850.0<br />

860.0<br />

730.0<br />

730.0<br />

720.0<br />

900.0<br />

880.0<br />

800.0<br />

890.0<br />

820.0<br />


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Sasp<br />

336 31<br />

337 31<br />

338 31<br />

339 31<br />

340 31<br />

341 32<br />

342 32<br />

343 32<br />

344 32<br />

345 32<br />

346 32<br />

347 32<br />

348 32<br />

349 32<br />

350 32<br />

351 32<br />

352 32<br />

353 32<br />

354 32<br />

355 33<br />

356 33<br />

357 33<br />

358 33<br />

359 33<br />

360 33<br />

361 33<br />

362 33<br />

363 33<br />

364 33<br />

365 33<br />

366 33<br />

367 33<br />

368 33<br />

369 33<br />

370 34<br />

371 34<br />

372 34<br />

373 34<br />

374 34<br />

375 34<br />

376 34<br />

377 34<br />

378 34<br />

379 34<br />

380 34<br />

381 34<br />

382 34<br />

383 34<br />

384 34<br />

385 34<br />

386 34<br />

387 35<br />

388 35<br />

389 35<br />

390 35<br />

391 35<br />

RNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

fiecor Hole Sasp<br />

392 35<br />

393 35<br />

394 35<br />

395 35<br />

396 35<br />

397 36<br />

398 36<br />

399 36<br />

400 36<br />

401 36<br />

402 36<br />

403 36<br />

404 36<br />

405 36<br />

406 36<br />

407 36<br />

408 36<br />

409 36<br />

410 36<br />

411 36<br />

412 36<br />

413 37<br />

414 37<br />

415 37<br />

416 37<br />

417 37<br />

418 37<br />

419 37<br />

420 37<br />

421 37<br />

422 37<br />

423 37<br />

424 37<br />

425 37<br />

426 37<br />

427 37<br />

428 37<br />

429 37<br />

430 37<br />

431 37<br />

432 37<br />

433 37<br />

434 37<br />

435 37<br />

436 36<br />

437 38<br />

438 38<br />

439 3B<br />

440 38<br />

441 38<br />

442 38<br />

443 38<br />

444 38<br />

445 38<br />

446 38<br />

447 38<br />

RNTBUSH OVERBURDEN DRILLING >>> H M C


i<br />

l<br />

l<br />

l<br />

l<br />

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l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Saip<br />

443 38<br />

449 38<br />

450 38<br />

451 36<br />

452 38<br />

453 39<br />

454 39<br />

455 39<br />

456 39<br />

457 39<br />

458 39<br />

459 39<br />

460 39<br />

461 39<br />

462 39<br />

463 39<br />

464 39<br />

465 39<br />

466 39<br />

467 39<br />

468 39<br />

469 39<br />

470 39<br />

471 40<br />

472 41<br />

473 41<br />

474 41<br />

475 41<br />

476 41<br />

477 41<br />

478 42<br />

479 42<br />

480 42<br />

481 42<br />

482 42<br />

483 42<br />

484 42<br />

485 42<br />

486 42<br />

487 43<br />

488 43<br />

489 43<br />

490 43<br />

491 43<br />

492 43<br />

493 43<br />

494 43<br />

495 44<br />

496 45<br />

497 45<br />

498 46<br />

499 46<br />

500 46<br />

501 47<br />

502 47<br />

503 47<br />

RNTBUSH OVERBURDEN DRILLING ><br />

*P<br />

13<br />

14<br />

15<br />

16<br />

17<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

21<br />

1<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

1<br />

1<br />

2<br />

1<br />

2<br />

3<br />

1<br />

2<br />

3<br />

Au<br />

39.0<br />

-11.0<br />

-10.0<br />

44.0<br />

4.0<br />

110.0<br />

140.0<br />

333.0<br />

92.0<br />

89.0<br />

150.0<br />

252.0<br />

140.0<br />

98.0<br />

190.0<br />

21.0<br />

448.0<br />

226.0<br />

-14.0<br />

264.0<br />

25.0<br />

-13.0<br />

3.0<br />

-2.0<br />

190.0<br />

-11.0<br />

69.0<br />

234.0<br />

-11.0<br />

8.0<br />

42.0<br />

46.0<br />

73.0<br />

71.0<br />

32.0<br />

333.0<br />

25.0<br />

-16.0<br />

6.0<br />

89.0<br />

20.0<br />

95.0<br />

120.0<br />

110.0<br />

34.0<br />

220,0<br />

11.0<br />

8.0<br />

200.0<br />

14.0<br />

47.0<br />

22.0<br />

4.0<br />

120.0<br />

140.0<br />

-18.0<br />

Cu<br />

116.0<br />

74.0<br />

64.0<br />

28.0<br />

0.0<br />

84.0<br />

132.0<br />

54.0<br />

116.0<br />

106.0<br />

100.0<br />

96.0<br />

124.0<br />

138.0<br />

218.0<br />

230.0<br />

230.0<br />

309.0<br />

268.0<br />

172.0<br />

106.0<br />

34.0<br />

0.0<br />

0.0<br />

54.0<br />

92.0<br />

108.0<br />

174.0<br />

206.0<br />

0.0<br />

86.0<br />

90.0<br />

96.0<br />

98.0<br />

88.0<br />

110.0<br />

98.0<br />

122.0<br />

0.0<br />

56.0<br />

224.0<br />

142.0<br />

168.0<br />

174.0<br />

110.0<br />

134.0<br />

0.0<br />

0.0<br />

62.0<br />

0.0<br />

108.0<br />

90.0<br />

0.0<br />

142.0<br />

72.0<br />

62.0<br />

As<br />

18.0<br />

26.0<br />

23.0<br />

33.0<br />

1.1<br />

8.2<br />

15.0<br />

22.0<br />

15.0<br />

20.0<br />

21.0<br />

27.0<br />

71.2<br />

30.0<br />

32.0<br />

35.0<br />

37.0<br />

44.0<br />

35.0<br />

42.0<br />

36.0<br />

14.0<br />

1.5<br />

-0.5<br />

5.4<br />

20.0<br />

31.0<br />

49.0<br />

43.0<br />

0.5<br />

28.0<br />

16.0<br />

20.0<br />

50.4<br />

23.0<br />

24.0<br />

24.0<br />

22.0<br />

0.9<br />

53.5<br />

20.0<br />

107.0<br />

38.0<br />

23.0<br />

29.0<br />

43.0<br />

1.7<br />

-0.5<br />

11.0<br />

1.6<br />

11.0<br />

14.0<br />

0.7<br />

31.0<br />

31.0<br />

18.0<br />

Sb<br />

0.4<br />

0.6<br />

0.6<br />

0.4<br />

0.3<br />

0.4<br />

0,5<br />

0.5<br />

0.5<br />

0.4<br />

0.5<br />

0.5<br />

0.6<br />

0.5<br />

0.6<br />

0.5<br />

0.5<br />

0.7<br />

0.7<br />

0.7<br />

0.8<br />

0.6<br />

0.1<br />

-0.1<br />

0.5<br />

0.6<br />

0.6<br />

0.5<br />

0.6<br />

-0.1<br />

0.5<br />

0.5<br />

0.4<br />

0.4<br />

0.5<br />

0.6<br />

0.5<br />

0.6<br />

0.2<br />

-0.2<br />

0.6<br />

0.7<br />

0.5<br />

0.6<br />

0.4<br />

0.7<br />

0.2<br />

0.1<br />

0.5<br />

0.4<br />

0.4<br />

0.5<br />

0.5<br />

0.4<br />

0.5<br />

0.5<br />

Ea<br />

-100.0<br />

-110.0<br />

-50.0<br />

-100.0<br />

550.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-110.0<br />

-110.0<br />

-110.0<br />

-120.0<br />

-120.0<br />

-120.0<br />

-130.0<br />

-120.0<br />

-110.0<br />

-120.0<br />

-130.0<br />

-130.0<br />

-120.0<br />

-120.0<br />

560.0<br />

120.0<br />

-110.0<br />

-100.0<br />

-110.0<br />

-50.0<br />

-100.0<br />

150.0<br />

-110.0<br />

-120.0<br />

-120.0<br />

-110.0<br />

-120.0<br />

-100.0<br />

-100.0<br />

-140.0<br />

230.0<br />

-130,0<br />

-110,0<br />

-110.0<br />

-50.0<br />

-100.0<br />

-110.0<br />

170.0<br />

600.0<br />

670.0<br />

-120.0<br />

170.0<br />

-130.0<br />

-120.0<br />

140.0<br />

-110.0<br />

-120.0<br />

-160.0<br />

Cd<br />

-15.0<br />

-16.0<br />

-14.0<br />

-16.0<br />

-5.0<br />

-14.0<br />

-14.0<br />

-15.0<br />

-16.0<br />

-16.0<br />

-17.0<br />

-18.0<br />

-17.0<br />

-18.0<br />

-20.0<br />

-18.0<br />

-17.0<br />

-17.0<br />

-20.0<br />

-19.0<br />

-18.0<br />

-19.0<br />

-5.0<br />

-5.0<br />

-16.0<br />

-15.0<br />

-17.0<br />

-15.0<br />

-16.0<br />

-5.0<br />

-16.0<br />

-19.0<br />

-18.0<br />

-18.0<br />

-18.0<br />

-16.0<br />

-16.0<br />

-23.0<br />

-5.0<br />

-20.0<br />

-16.0<br />

-17.0<br />

-15.0<br />

-16.0<br />

-18.0<br />

-17.0<br />

-5,0<br />

-5.0<br />

-19.0<br />

-5.0<br />

-20.0<br />

-19.0<br />

-5.0<br />

-17.0<br />

-20.0<br />

-26.0<br />

>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Reeor Hole Sasp<br />

504 47<br />

505 47<br />

506 47<br />

507 47<br />

508 48<br />

509 48<br />

510 49<br />

511 49<br />

512 49<br />

513 49<br />

514 49<br />

515 50<br />

516 51<br />

517 51<br />

518 51<br />

519 51<br />

520 52<br />

521 52<br />

522 52<br />

523 53<br />

524 53<br />

525 54<br />

526 54<br />

527 54<br />

528 54<br />

529 55<br />

530 55<br />

531 55<br />

532 55<br />

533 55<br />

534 55<br />

535 55<br />

536 55<br />

537 56<br />

538 56<br />

539 56<br />

540 56<br />

541 56<br />

542 57<br />

543 57<br />

544 57<br />

545 58<br />

546 56<br />

547 58<br />

548 58<br />

549 59<br />

550 59<br />

551 59<br />

552 59<br />

553 59<br />

554 59<br />

555 60<br />

556 60<br />

557 60<br />

558 60<br />

559 60<br />

^NTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

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l<br />

Page 11 of BURNTBUSH OVERBURDEN DRILLING >>> H M C [87/12/22]<br />

Recor Hole Satp Au Cu As Sb Da Cd Cs Cr Co Eu Hf Ir<br />

560<br />

561<br />

562<br />

563<br />

564<br />

565<br />

566<br />

567<br />

568<br />

569<br />

570<br />

571<br />

572<br />

573<br />

574<br />

575<br />

576<br />

577<br />

578<br />

579<br />

580<br />

581<br />

582<br />

583<br />

584<br />

585<br />

586<br />

587<br />

588<br />

589<br />

590<br />

591<br />

592<br />

593<br />

594<br />

595<br />

596<br />

597<br />

598<br />

599<br />

600<br />

601<br />

602<br />

603<br />

604<br />

605<br />

606<br />

607<br />

608<br />

609<br />

610<br />

611<br />

612<br />

613<br />

614<br />

615<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

61<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

62<br />

63<br />

63<br />

64<br />

64<br />

64<br />

64<br />

65<br />

65<br />

65<br />

65<br />

65<br />

66<br />

66<br />

67<br />

67<br />

67<br />

67<br />

67<br />

67<br />

67<br />

67<br />

6B<br />

69<br />

70<br />

70<br />

70<br />

71<br />

72<br />

72<br />

72<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

1<br />

1<br />

2<br />

3<br />

1<br />

1<br />

2<br />

3<br />

40.0<br />

329.0<br />

63.0<br />

64.0<br />

68.0<br />

17.0<br />

110.0<br />

-8.0<br />

120.0<br />

36.0<br />

289.0<br />

130.0<br />

4860.0<br />

9.0<br />

58.0<br />

-7.0<br />

120.0<br />

100.0<br />

-8.0<br />

83.0<br />

45.0<br />

20.0<br />

26.0<br />

201.0<br />

231.0<br />

-2.0<br />

120.0<br />

-2,0<br />

32.0<br />

80.0<br />

5400.0<br />

-2.0<br />

423.0<br />

120.0<br />

1790.0<br />

68.0<br />

12.0<br />

14.0<br />

-2.0<br />

120.0<br />

19.0<br />

18.0<br />

-2.0<br />

1310.0<br />

35.0<br />

251.0<br />

13.0<br />

7.0<br />

5.0<br />

22.0<br />

13,0<br />

-2.0<br />

3.0<br />

293.0<br />

545.0<br />

524.0<br />

102.0<br />

120.0<br />

158.0<br />

116.0<br />

102.0<br />

132.0<br />

124.0<br />

72.0<br />

74.0<br />

56.0<br />

40.0<br />

202.0<br />

129.0<br />

0.0<br />

68.0<br />

40.0<br />

110.0<br />

96.0<br />

80.0<br />

88.0<br />

108.0<br />

156.0<br />

82,0<br />

56.0<br />

82.0<br />

0.0<br />

184.0<br />

0.0<br />

34.0<br />

98.0<br />

46.0<br />

0.0<br />

42.0<br />

66.0<br />

100.0<br />

324.0<br />

0.0<br />

44.0<br />

0,0<br />

518.0<br />

100.0<br />

118.0<br />

0.0<br />

120.0<br />

176.0<br />

54.0<br />

0.0<br />

0.0<br />

0.0<br />

182.0<br />

202.0<br />

0.0<br />

0.0<br />

58.0<br />

94.0<br />

30.0<br />

3.4<br />

15.0<br />

21.0<br />

13.0<br />

18.0<br />

19.0<br />

29.0<br />

15.0<br />

13.0<br />

10.0<br />

14.0<br />

11.0<br />

26.0<br />

0.7<br />

45.0<br />

43.0<br />

54.8<br />

52.2<br />

53.9<br />

113.0<br />

51.9<br />

47.0<br />

36.0<br />

41.0<br />

47.0<br />

1.3<br />

27.0<br />

-0.5<br />

7.8<br />

22.0<br />

19.0<br />

0.6<br />

18.0<br />

5.0<br />

6,3<br />

4.0<br />

1.0<br />

12.0<br />

2.5<br />

22.0<br />

33.0<br />

25.0<br />

-0.5<br />

42.0<br />

54.6<br />

49.0<br />

-0.5<br />

-0.5<br />

-0.5<br />

3.2<br />

-2.2<br />

-0.5<br />

-0.5<br />

-2.5<br />

21.0<br />

13.0<br />

0.3<br />

0.4<br />

0.6<br />

0.5<br />

0.6<br />

0.4<br />

0.5<br />

0.6<br />

0.5<br />

0.5<br />

0.4<br />

0.4<br />

0.7<br />

-0.1<br />

0.5<br />

0.4<br />

0.5<br />

0.6<br />

0.7<br />

1.4<br />

0.5<br />

0.8<br />

0.7<br />

0.6<br />

0.6<br />

-0.1<br />

0.6<br />

-0.1<br />

0.3<br />

0.6<br />

0.4<br />

-0.1<br />

0.4<br />

0.5<br />

0.3<br />

0.2<br />

0.1<br />

0.4<br />

0.1<br />

0.4<br />

0.6<br />

0.6<br />

0.1<br />

0.6<br />

0.7<br />

0.6<br />

-0.1<br />

-0.1<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

-O.I<br />

0.1<br />

0.4<br />

0.3<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

83.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

120.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

62.0<br />

380.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

130.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

340.0<br />

-50.0<br />

230.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

320.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

390.0<br />

-50.0<br />

860.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

310.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

230.0<br />

210.0<br />

210.0<br />

-50.0<br />

71.0<br />

300.0<br />

930.0<br />

81.0<br />

-50.0<br />

-50.0<br />

-13.0<br />

-14.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-10.0<br />

-11.0<br />

-12.0<br />

-5.0<br />

-11.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-12.0<br />

-11.0<br />

-5.0<br />

-5.0<br />

-12.0<br />

-5.0<br />

-11.0<br />

-5.0<br />

-11.0<br />

-10.0<br />

-11.0<br />

-5.0<br />

-11.0<br />

-5.0<br />

-11.0<br />

-11.0<br />

-13.0<br />

-5.0<br />

-10.0<br />

-11.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-13.0<br />

-5.0<br />

-13.0<br />

-16.0<br />

-14.0<br />

-5.0<br />

-16.0<br />

-14.0<br />

-14.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-12.0<br />

20.0<br />

-0.5<br />

-0.5<br />

-0.5<br />

0.6<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.1<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

2.1<br />

-0.5<br />

1.1<br />

-0.5<br />

-0.5<br />

-0.5<br />

4.3<br />

-0.5<br />

-0.5<br />

0.8<br />

0.6<br />

0.8<br />

-0.5<br />

1.4<br />

0.9<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

1.9<br />

1.0<br />

1.8<br />

0.5<br />

0.8<br />

1.2<br />

2.9<br />

1.0<br />

-0.5<br />

-1.1<br />

910.0<br />

940.0<br />

790.0<br />

980.0<br />

800.0<br />

920.0<br />

1000.0<br />

1100.0<br />

1100.0<br />

1100.0<br />

1200.0<br />

820.0<br />

690.0<br />

170.0<br />

1300.0<br />

1100.0<br />

1000.0<br />

1000.0<br />

1200.0<br />

820.0<br />

1200.0<br />

890.0<br />

880.0<br />

870.0<br />

900.0<br />

57.0<br />

890.0<br />

120.0<br />

1200.0<br />

870.0<br />

1000.0<br />

120.0<br />

910.0<br />

950.0<br />

710.0<br />

680.0<br />

260.0<br />

1000.0<br />

230.0<br />

960.0<br />

1200.0<br />

1000.0<br />

230.0<br />

1200.0<br />

1100.0<br />

1100.0<br />

110.0<br />

150.0<br />

150.0<br />

530.0<br />

360.0<br />

150.0<br />

190.0<br />

470.0<br />

1000.0<br />

1100.0<br />

73.0<br />

110.0<br />

150.0<br />

140.0<br />

150.0<br />

150.0<br />

150.0<br />

87.0<br />

88.0<br />

78.0<br />

57.0<br />

170.0<br />

130.0<br />

13.0<br />

120.0<br />

99.0<br />

150.0<br />

110.0<br />

140.0<br />

190.0<br />

140.0<br />

130.0<br />

110.0<br />

100.0<br />

100.0<br />

35.0<br />

130.0<br />

21.0<br />

55.0<br />

160.0<br />

93.0<br />

36.0<br />

98.0<br />

95.0<br />

86.0<br />

68.0<br />

34.0<br />

56.0<br />

14.0<br />

210.0<br />

83.0<br />

100.0<br />

51.0<br />

150.0<br />

180.0<br />

120.0<br />

46.0<br />

18.0<br />

19.0<br />

150.0<br />

190.0<br />

33.0<br />

10.0<br />

200.0<br />

75.0<br />

51.0<br />

5.0<br />

9.0<br />

7.0<br />

8.0<br />

7.0<br />

7.0<br />

9.0<br />

12.0<br />

10.0<br />

9.0<br />

9.0<br />

15.0<br />

5.0<br />

-1.0<br />

10.0<br />

8.0<br />

10.0<br />

e.o<br />

8.0<br />

5.0<br />

7.0<br />

7.0<br />

7.0<br />

8.0<br />

8.0<br />

1.0<br />

11.0<br />

2.0<br />

9.0<br />

9.0<br />

12.0<br />

1.0<br />

8.0<br />

9.0<br />

7.0<br />

6.0<br />

-1.0<br />

13.0<br />

2.0<br />

11.0<br />

16.0<br />

8.0<br />

-1.0<br />

9.0<br />

10.0<br />

8.0<br />

1.0<br />

2.0<br />

1.0<br />

10.0<br />

2.0<br />

-1.0<br />

-1.0<br />

6.0<br />

10.0<br />

13.0<br />

299.0<br />

323.0<br />

257.0<br />

297.0<br />

258.0<br />

252.0<br />

280.0<br />

294.0<br />

382.0<br />

279.0<br />

309.0<br />

117.0<br />

103.0<br />

4.0<br />

337.0<br />

338.0<br />

303.0<br />

262.0<br />

335.0<br />

167.0<br />

316.0<br />

171.0<br />

246.0<br />

228.0<br />

235.0<br />

5.0<br />

179.0<br />

6.0<br />

240.0<br />

279.0<br />

270.0<br />

5.0<br />

206.0<br />

146.0<br />

94.0<br />

58.0<br />

4.0<br />

280.0<br />

4.0<br />

264.0<br />

398.0<br />

328.0<br />

2.0<br />

373.0<br />

286.0<br />

291.0<br />

3.0<br />

9.0<br />

7.0<br />

61.0<br />

7.0<br />

3.0<br />

4.0<br />

33.0<br />

319.0<br />

322.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50,0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0


l l<br />

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Page<br />

12 of<br />

Recor Hole Satp<br />

616 72<br />

617 73<br />

618 73<br />

619 74<br />

620 H<br />

621 74<br />

622 75<br />

623 76<br />

624 77<br />

625 77<br />

626 77<br />

627 77<br />

628 78<br />

629 78<br />

630 78<br />

631 78<br />

632 78<br />

633 78<br />

634 79<br />

635 79<br />

636 79<br />

637 80<br />

638 60<br />

639 81<br />

640 82<br />

641 82<br />

642 82<br />

643 82<br />

644 82<br />

645 82<br />

646 82<br />

647 82<br />

648 82<br />

649 82<br />

650 82<br />

651 82<br />

652 82<br />

653 83<br />

654 83<br />

655 84<br />

656 84<br />

657 84<br />

658 84<br />

659 84<br />

660 84<br />

661 84<br />

662 84<br />

663 85<br />

664 85<br />

665 85<br />

666 85<br />

667 85<br />

668 85<br />

669 85<br />

670 85<br />

671 85<br />

RNTBUSH OVERBURDEN DRILLING ><br />

sp<br />

4<br />

1<br />

2<br />

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2<br />

3<br />

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3<br />

4<br />

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4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

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2<br />

3<br />

4<br />

5<br />

6<br />

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g<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

Au<br />

-2.0<br />

14.0<br />

6.0<br />

130.0<br />

1240.0<br />

-2.0<br />

-2.0<br />

9.0<br />

140.0<br />

61.0<br />

15.0<br />

10.0<br />

110.0<br />

505,0<br />

25.0<br />

95.0<br />

229.0<br />

3.0<br />

247.0<br />

33.0<br />

-2.0<br />

266.0<br />

28.0<br />

2.0<br />

1140.0<br />

37.0<br />

64.0<br />

. 53.0<br />

170.0<br />

32.0<br />

1020.0<br />

- 65.0<br />

130.0<br />

26.0<br />

100.0<br />

16.0<br />

8.0<br />

234.0<br />

-2.0<br />

130.0<br />

120.0<br />

51.0<br />

40.0<br />

130.0<br />

42,0<br />

110.0<br />

17.0<br />

160.0<br />

84.0<br />

618.0<br />

45.0<br />

258.0<br />

160.0<br />

474.0<br />

59.0<br />

160.0<br />

Cu<br />

0.0<br />

94.0<br />

0.0<br />

80.0<br />

46.0<br />

0.0<br />

0.0<br />

0.0<br />

68.0<br />

46.0<br />

0.0<br />

0.0<br />

60.0<br />

102.0<br />

72.0<br />

70.0<br />

84.0<br />

0.0<br />

30.0<br />

68.0<br />

0.0<br />

108.0<br />

26.0<br />

5.0<br />

78.0<br />

130.0<br />

60.0<br />

56.0<br />

86.0<br />

120.0<br />

108.0<br />

68.0<br />

58.0<br />

56.0<br />

112.0<br />

64.0<br />

9.0<br />

68.0<br />

3.0<br />

82.0<br />

56.0<br />

56.0<br />

126.0<br />

138.0<br />

180.0<br />

158.0<br />

123.0<br />

86.0<br />

64.0<br />

68.0<br />

48.0<br />

106.0<br />

114.0<br />

102.0<br />

68.0<br />

122.0<br />

As<br />

-0.5<br />

16.0<br />

1.8<br />

17.0<br />

18.0<br />

0.9<br />

1.0<br />

0.7<br />

27.0<br />

15.0<br />

2.1<br />

2.0<br />

16.0<br />

114.0<br />

17.0<br />

26.0<br />

23.0<br />

-0.5<br />

9.0<br />

10.0<br />

-0.5<br />

62.6<br />

4.9<br />

-0.5<br />

20.0<br />

20.0<br />

128.0<br />

10.0<br />

22.0<br />

27.0<br />

17.0<br />

18.0<br />

8.7<br />

14.0<br />

21.0<br />

24.0<br />

4.5<br />

29.0<br />

0.7<br />

22.0<br />

31.0<br />

20.0<br />

26.0<br />

30.0<br />

41.0<br />

42.0<br />

0.8<br />

24.0<br />

21.0<br />

15.0<br />

17.0<br />

45.0<br />

63.4<br />

54.7<br />

34.0<br />

78.5<br />

Sb<br />

0.1<br />

0.3<br />

0.2<br />

0.3<br />

0.4<br />

-0.1<br />

-0.1<br />

0.6<br />

0.5<br />

0.5<br />

0.6<br />

0.3<br />

0.5<br />

0.5<br />

0.5<br />

0.4<br />

0.8<br />

0.3<br />

0.4<br />

0.4<br />

0.4<br />

0.7<br />

0.8<br />

0.2<br />

0.6<br />

0.5<br />

0.5<br />

0.4<br />

0.4<br />

0.6<br />

0.4<br />

0.5<br />

0.3<br />

0.3<br />

0.7<br />

0.6<br />

0.6<br />

0.7<br />

0.4<br />

0.4<br />

0.6<br />

0.6<br />

0.5<br />

0.6<br />

1.0<br />

0.7<br />

0.2<br />

0.4<br />

0.3<br />

0.4<br />

0.6<br />

0.6<br />

1.0<br />

0.7<br />

0.5<br />

0.8<br />

Ea<br />

110.0<br />

-50.0<br />

330.0<br />

-50.0<br />

-50.0<br />

290.0<br />

470.0<br />

1200.0<br />

-50.0<br />

-50.0<br />

1500.0<br />

1100.0<br />

110.0<br />

82.0<br />

120.0<br />

-50.0<br />

-50.0<br />

1300.0<br />

-50.0<br />

-50.0<br />

1500.0<br />

-50.0<br />

860.0<br />

1300.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

1300.0<br />

-50.0<br />

1500.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

750.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

Cd<br />

-5.0<br />

-14.0<br />

-5.0<br />

-12,0<br />

-14.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-13.0<br />

-13.0<br />

-5.0<br />

-5.0<br />

-12.0<br />

-11.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

-5.0<br />

-12.0<br />

-11.0<br />

-5.0<br />

-14.0<br />

-5.0<br />

-5.0<br />

-13.0<br />

-12.0<br />

-13.0<br />

-13.0<br />

-12.0<br />

-16.0<br />

-14.0<br />

13.0<br />

-12.0<br />

-13,0<br />

-17.0<br />

-16.0<br />

-5.0<br />

-15.0<br />

-5,0<br />

-15,0<br />

-15.0<br />

-18.0<br />

-13,0<br />

-12,0<br />

-13.0<br />

-13.0<br />

-5,0<br />

-15,0<br />

-14,0<br />

-14.0<br />

-16.0<br />

-22,0<br />

-12,0<br />

-11.0<br />

-11.0<br />

-13.0<br />

>> H M c


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Recor Hole Saip<br />

672 85<br />

673 86<br />

674 86<br />

675 66<br />

676 86<br />

677 86<br />

678 86<br />

679 87<br />

680 87<br />

681 87<br />

682 87<br />

683 88<br />

684 88<br />

685 88<br />

686 88<br />

687 88<br />

688 88<br />

689 ' 88<br />

690 89<br />

691 89<br />

692 89<br />

693 89<br />

694 89<br />

695 89<br />

696 89<br />

697 89<br />

698 89<br />

699 89<br />

700 89<br />

701 90<br />

702 90<br />

703 90<br />

704 90<br />

705 90<br />

706 90<br />

707 90<br />

708 90<br />

709 90<br />

710 90<br />

711 90<br />

712 90<br />

713 90<br />

714 90<br />

715 90<br />

716 91<br />

717 91<br />

718 91<br />

719 91<br />

720 91<br />

721 91<br />

722 91<br />

723 91<br />

724 92<br />

725 92<br />

726 92<br />

727 92<br />

RNTBUSH OVERBURDEN DRILLING > >> H M C


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Page 14 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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Recor Hole Sasp<br />

784 98<br />

785 98<br />

786 98<br />

787 98<br />

788 98<br />

789 98<br />

790 98<br />

791 98<br />

792 98<br />

793 98<br />

794 98<br />

795 99<br />

796 99<br />

797 99<br />

798 99<br />

799 99<br />

800 100<br />

801 100<br />

802 100<br />

803 100<br />

804 100<br />

805 100<br />

606 100<br />

607 100<br />

808 100<br />

809 100<br />

810 100<br />

811 100<br />

812 100<br />

813 100<br />

814 100<br />

815 100<br />

816 100<br />

817 100<br />

818 100<br />

819 101<br />

820 101<br />

821 101<br />

822 101<br />

823 101<br />

824 101<br />

825 101<br />

826 101<br />

827 101<br />

828 101<br />

829 101<br />

830 101<br />

831 101<br />

832 101<br />

833 101<br />

834 101<br />

835 102<br />

836 102<br />

837 102<br />

838 102<br />

839 102<br />

RNTBUSH OVERBURDEN DRILLING >>><br />

t?<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

11<br />

12<br />

13<br />

1<br />

2<br />

3<br />

4<br />

5<br />

i<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

e<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

i<br />

2<br />

3<br />

4<br />

5<br />

Au<br />

130.0<br />

-21.0<br />

39.0<br />

73.0<br />

42.0<br />

190.0<br />

425.0<br />

29.0<br />

511.0<br />

335.0<br />

8.0<br />

25.0<br />

279.0<br />

B9.0<br />

540.0<br />

3.0<br />

623.0<br />

96.0<br />

45.0<br />

57.0<br />

76.0<br />

110.0<br />

110.0<br />

234.0<br />

86.0<br />

66.0<br />

140.0<br />

206.0<br />

233.0<br />

40.0<br />

77.0<br />

160.0<br />

82.0<br />

37.0<br />

-2.0<br />

23.0<br />

42.0<br />

46.0<br />

490.0<br />

405.0<br />

66.0<br />

-12.0<br />

345.0<br />

44.0<br />

-12.0<br />

82,0<br />

85.0<br />

50.0<br />

1030.0<br />

140.0<br />

-2.0<br />

33.0<br />

130.0<br />

120.0<br />

211.0<br />

-13.0<br />

Cu<br />

87.0<br />

101.0<br />

82.0<br />

78.0<br />

102.0<br />

122.0<br />

94.0<br />

89.0<br />

90.0<br />

90.0<br />

26.0<br />

28.0<br />

30.0<br />

104.0<br />

165.0<br />

46.0<br />

18.0<br />

36.0<br />

94.0<br />

111.0<br />

100.0<br />

132.0<br />

104.0<br />

122.0<br />

158.0<br />

195.0<br />

170.0<br />

136.0<br />

116.0<br />

96.0<br />

98.0<br />

134.0<br />

54.0<br />

66.0<br />

50.0<br />

64.0<br />

110.0<br />

104.0<br />

74.0<br />

86.0<br />

112.0<br />

155.0<br />

102.0<br />

154.0<br />

141.0<br />

134.0<br />

94.0<br />

84.0<br />

B8.G<br />

84.0<br />

7.0<br />

34.0<br />

18.0<br />

110.0<br />

75.0<br />

262.0<br />

As<br />

19.0<br />

15.0<br />

18.0<br />

27.0<br />

14.0<br />

21.0<br />

20.0<br />

17.0<br />

18.0<br />

13.0<br />

0.7<br />

18.0<br />

-4.0<br />

15.0<br />

30.0<br />

1.0<br />

4.0<br />

6.0<br />

17.0<br />

17.0<br />

19.0<br />

18.0<br />

15.0<br />

14.0<br />

17.0<br />

29.0<br />

28.0<br />

25.0<br />

17.0<br />

13.0<br />

20.0<br />

16.0<br />

10.0<br />

21.0<br />

-0.5<br />

29.0<br />

15.0<br />

17.0<br />

13.0<br />

21.0<br />

30.0<br />

16.0<br />

17.0<br />

16.0<br />

25.0<br />

13.0<br />

20.0<br />

16.0<br />

21.0<br />

32.0<br />

1.6<br />

7.0<br />

-5.6<br />

-4.9<br />

-4.9<br />

20.0<br />

Sb<br />

-0.3<br />

0.5<br />

0.7<br />

0.4<br />

0.6<br />

0.5<br />

-0.3<br />

0.4<br />

0.4<br />

-0.2<br />

0.1<br />

0.4<br />

-0.2<br />

0.6<br />

0.5<br />

-0.1<br />

0.4<br />

1.2<br />

0.5<br />

0.4<br />

1.3<br />

0.4<br />

-0.2<br />

0.4<br />

0.5<br />

0.5<br />

0.5<br />

0.4<br />

0.6<br />

0.6<br />

0.5<br />

0.8<br />

-0.2<br />

0.5<br />

0.1<br />

-0.2<br />

0.4<br />

0.4<br />

0.5<br />

0.5<br />

0.4<br />

0.3<br />

0.5<br />

0.5<br />

1.0<br />

0.4<br />

0.7<br />

0.4<br />

0.3<br />

0.6<br />

0.1<br />

0.5<br />

-0.2<br />

0.4<br />

0.4<br />

0.4<br />

6a<br />

-110.0<br />

-120.0<br />

-120.0<br />

-110.0<br />

-120.0<br />

-140.0<br />

-130.0<br />

-100.0<br />

-110.0<br />

-120.0<br />

250.0<br />

-130.0<br />

-120.0<br />

-120.0<br />

-130.0<br />

320.0<br />

-120.0<br />

-120.0<br />

-120.0<br />

-130.0<br />

-120.0<br />

-120.0<br />

-140.0<br />

180.0<br />

-130.0<br />

-130.0<br />

-120.0<br />

-120.0<br />

-100.0<br />

-100.0<br />

-110.0<br />

-110.0<br />

-110.0<br />

200.0<br />

150.0<br />

-120.0<br />

-120.0<br />

200.0<br />

-120.0<br />

-120.0<br />

-120.0<br />

-110.0<br />

-100.0<br />

-120.0<br />

-110.0<br />

-100.0<br />

-120.0<br />

-120.0<br />

-110.0<br />

-120.0<br />

1200.0<br />

-130.0<br />

-130.0<br />

-120.0<br />

230.0<br />

-120.0<br />

Cd<br />

-20.0<br />

-20.0<br />

-22.0<br />

-20.0<br />

-21.0<br />

-23.0<br />

-21.0<br />

-15.0<br />

-17.0<br />

-17.0<br />

-5.0<br />

-19.0<br />

-18.0<br />

-17.0<br />

-18.0<br />

-5.0<br />

-18.0<br />

-18.0<br />

-18.0<br />

-16.0<br />

-17.0<br />

-17.0<br />

-20.0<br />

-18.0<br />

-18.0<br />

-19.0<br />

-18.0<br />

-18.0<br />

-15.0<br />

-14.0<br />

-16.0<br />

-17.0<br />

-16.0<br />

-16.0<br />

-5.0<br />

-19.0<br />

-17.0<br />

-19.0<br />

-18.0<br />

-18.0<br />

-19.0<br />

-16.0<br />

-15.0<br />

-18.0<br />

-17.0<br />

20.0<br />

-18.0<br />

20.0<br />

-17.0<br />

24.0<br />

-5.0<br />

-22.0<br />

-22.0<br />

-19.0<br />

-19.0<br />

-19.0<br />

H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Easp<br />

840 102<br />

641 102<br />

842 102<br />

843 102<br />

844 102<br />

645 102<br />

846 102<br />

847 102<br />

648 102<br />

849 103<br />

850 103<br />

851 103<br />

852 103<br />

853 103<br />

854 103<br />

855 103<br />

856 103<br />

857 103<br />

858 103<br />

859 103<br />

860 103<br />

861 103<br />

862 103<br />

863 103<br />

864 103<br />

865 103<br />

866 103<br />

867 104<br />

868 104<br />

869 104<br />

870 104<br />

871 104<br />

872 104<br />

873 104<br />

874 104<br />

875 104<br />

876 104<br />

877 104<br />

878 104<br />

879 104<br />

830 104<br />

881 104<br />

682 104<br />

883 104<br />

884 104<br />

835 104<br />

886 104<br />

887 105<br />

888 105<br />

689 105<br />

890 105<br />

891 105<br />

892 105<br />

893 105<br />

894 105<br />

895 105<br />

RNTBUSH OVERBURDEN DRILLING >>> H M C


l l<br />

l<br />

l<br />

l l<br />

l l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l l<br />

l<br />

l<br />

Page<br />

17 of<br />

Recor Hole Saip<br />

896 106<br />

897 106<br />

898 106<br />

899 106<br />

900 106<br />

901 106<br />

902 106<br />

903 106<br />

904 106<br />

905 106<br />

906 106<br />

907 106<br />

908 106<br />

909 106<br />

910 106<br />

911 106<br />

912 106<br />

913 106<br />

914 107<br />

915 107<br />

916 107<br />

917 107<br />

918 107<br />

919 107<br />

920 107<br />

921 107<br />

922 107<br />

923 107<br />

924 107<br />

925 107<br />

926 107<br />

927 107<br />

928 107<br />

929 107<br />

930 107<br />

931 107<br />

932 107<br />

933 107<br />

934 107<br />

935 107<br />

936 107<br />

937 108<br />

938 108<br />

939 108<br />

940 108<br />

941 108<br />

942 108<br />

943 108<br />

944 108<br />

945 108<br />

946 108<br />

947 108<br />

948 108<br />

949 108<br />

950 108<br />

951 109<br />

RNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

fiecor Hole Sacp<br />

952 109<br />

953 109<br />

954 109<br />

955 109<br />

956 109<br />

957 109<br />

958 109<br />

959 109<br />

960 109<br />

961 109<br />

962 109<br />

963 109<br />

964 109<br />

965 109<br />

966 109<br />

967 109<br />

968 109<br />

969 109<br />

970 109<br />

971 110<br />

972 110<br />

973 110<br />

974 110<br />

975 110<br />

976 110<br />

977 110<br />

978 110<br />

979 110<br />

980 110<br />

981 110<br />

982 110<br />

983 110<br />

984 111<br />

985 111<br />

986 111<br />

987 111<br />

988 111<br />

989 111<br />

990 111<br />

991 111<br />

992 111<br />

993 111<br />

994 111<br />

995 111<br />

996 112<br />

997 112<br />

998 112<br />

999 112<br />

1000 112<br />

1001 112<br />

1002 112<br />

1003 113<br />

1004 113<br />

1005 113<br />

1006 113<br />

1007 113<br />

RNTBUSH OVERBURDEN DRILLING >>><br />

*P<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

H<br />

12<br />

13<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

Au<br />

72.0<br />

190.0<br />

303.0<br />

100.0<br />

48.0<br />

219.0<br />

35.0<br />

60.0<br />

95.0<br />

160.0<br />

-17.0<br />

-17.0<br />

54,0<br />

110.0<br />

33.0<br />

61.0<br />

56.0<br />

140.0<br />

-2.0<br />

54.0<br />

47.0<br />

2610.0<br />

62.0<br />

709.0<br />

30.0<br />

75.0<br />

63.0<br />

390.0<br />

652.0<br />

95.0<br />

390.0<br />

-2.0<br />

89.0<br />

61.0<br />

51.0<br />

45.0<br />

140.0<br />

37.0<br />

230.0<br />

65.0<br />

41.0<br />

48.0<br />

44.0<br />

6.0<br />

190.0<br />

57.0<br />

64.0<br />

280.0<br />

26.0<br />

-20.0<br />

-2.0<br />

260.0<br />

120.0<br />

66.0<br />

375.0<br />

92.0<br />

Cu<br />

123.0<br />

75.0<br />

50.0<br />

73.0<br />

52.0<br />

45.0<br />

12.0<br />

32.0<br />

53.0<br />

78.0<br />

120.0<br />

114.0<br />

110.0<br />

150.0<br />

171.0<br />

95.0<br />

92.0<br />

79.0<br />

48.0<br />

54.0<br />

79.0<br />

91.0<br />

110.0<br />

162.0<br />

119.0<br />

9.0<br />

35.0<br />

60.0<br />

114.0<br />

160.0<br />

162.0<br />

35.0<br />

140.0<br />

130.0<br />

156.0<br />

145.0<br />

128.0<br />

138.0<br />

146.0<br />

128.0<br />

189.0<br />

173.0<br />

106.0<br />

30.0<br />

187.0<br />

157.0<br />

165.0<br />

148.0<br />

108.0<br />

163.0<br />

70.0<br />

13.0<br />

39.0<br />

20.0<br />

70.0<br />

64.0<br />

As<br />

24.0<br />

18.0<br />

18.0<br />

43.0<br />

12.0<br />

-6.2<br />

6.7<br />

-6.1<br />

-6.0<br />

15.0<br />

33.0<br />

46.0<br />

30.0<br />

33.0<br />

20.0<br />

95.0<br />

142.0<br />

41.0<br />

0.9<br />

31.0<br />

16.0<br />

12.0<br />

-10.0<br />

13.0<br />

17.0<br />

-10.0<br />

-11.0<br />

-12.0<br />

-11.0<br />

59.0<br />

99.0<br />

-0.5<br />

33.0<br />

12.0<br />

15.0<br />

28.0<br />

19.0<br />

17.0<br />

22.0<br />

17.0<br />

28.0<br />

17.0<br />

23.0<br />

1.1<br />

22.0<br />

16.0<br />

29.0<br />

24.0<br />

14.0<br />

17.0<br />

-0.5<br />

-10.0<br />

-11.0<br />

-6.4<br />

-6.7<br />

9.5<br />

Sfa<br />

0.7<br />

0.4<br />

0.5<br />

0.6<br />

0.6<br />

-0.2<br />

0.6<br />

0.4<br />

0.4<br />

-0.2<br />

0.6<br />

0.5<br />

0.7<br />

0.4<br />

0.4<br />

0.8<br />

1.0<br />

0.4<br />

-0.1<br />

0.6<br />

0.5<br />

0.5<br />

-0.2<br />

0.5<br />

0.8<br />

-0.2<br />

-0.2<br />

0.6<br />

0.5<br />

0.6<br />

0.7<br />

0.1<br />

0.5<br />

0.4<br />

0.6<br />

0.6<br />

-0.2<br />

0.5<br />

0.5<br />

0.4<br />

0.6<br />

0.5<br />

0.9<br />

-0.1<br />

0.6<br />

-0.2<br />

0.6<br />

-0.2<br />

0.6<br />

0.5<br />

-0.1<br />

0.5<br />

0.5<br />

0.4<br />

0.6<br />

0.5<br />

Ba<br />

-150.0<br />

-120.0<br />

-140.0<br />

-120.0<br />

-130.0<br />

-150.0<br />

-140.0<br />

-150.0<br />

-140.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

280.0<br />

-100.0<br />

860.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

790.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

180.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

1100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

1300.0<br />

-100.0<br />

-100.0<br />

-140.0<br />

-150.0<br />

-150.0<br />

Cd<br />

-25.0<br />

-23.0<br />

-23.0<br />

-23.0<br />

-22.0<br />

-24.0<br />

-23.0<br />

-24.0<br />

-24.0<br />

-28.0<br />

-31.0<br />

-29.0<br />

-30.0<br />

-29.0<br />

-28.0<br />

-31.0<br />

-30.0<br />

-31.0<br />

-5.0<br />

-37.0<br />

-33.0<br />

-30.0<br />

-31.0<br />

-31.0<br />

-31.0<br />

-31.0 .<br />

-33.0<br />

-35.0<br />

-34.0<br />

-26.0<br />

-32.0<br />

-5.0<br />

-31.0<br />

-31.0<br />

-33.0<br />

-33.0<br />

-31.0<br />

-31.0<br />

-32.0<br />

-31.0<br />

-31.0<br />

-32.0<br />

-32.0<br />

-5.0<br />

-34.0<br />

-32.0<br />

-34.0<br />

-32.0<br />

-31.0<br />

-31.0<br />

-5.0<br />

-29.0<br />

-33.0<br />

-24.0<br />

-26.0<br />

-25.0<br />

H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

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Page 19 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

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l<br />

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age<br />

20 of BURNTBUSH<br />

ecor<br />

1064<br />

1065<br />

1066<br />

1067<br />

1068<br />

1069<br />

1070<br />

1071<br />

1072<br />

1073<br />

1074<br />

1075<br />

1076<br />

1077<br />

1078<br />

1079<br />

1080<br />

1081<br />

1082<br />

1083<br />

1084<br />

1085<br />

1086<br />

1087<br />

1088<br />

1089<br />

1090<br />

1091<br />

1092<br />

1093<br />

1094<br />

1095<br />

1096<br />

1097<br />

1098<br />

1099<br />

1100<br />

1101<br />

1102<br />

1103<br />

1104<br />

1105<br />

1106<br />

1107<br />

1108<br />

1109<br />

1110<br />

1111<br />

1112<br />

1113<br />

1114<br />

1115<br />

1116<br />

1117<br />

1118<br />

1119<br />

Hole<br />

118<br />

118<br />

118<br />

118<br />

119<br />

119<br />

120<br />

120<br />

121<br />

121<br />

122<br />

122<br />

122<br />

122<br />

122<br />

122<br />

122<br />

122<br />

122<br />

122<br />

123<br />

123<br />

123<br />

123<br />

123<br />

123<br />

123<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

124<br />

125<br />

125A<br />

125A<br />

125A<br />

126<br />

126<br />

126<br />

126<br />

126<br />

126<br />

127<br />

127<br />

Saep<br />

5<br />

6<br />

7<br />

B<br />

1<br />

2<br />

1<br />

2<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7 e 9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

1<br />

1<br />

2<br />

3<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

Au<br />

66.0<br />

15.0<br />

130.0<br />

-2.0<br />

16.0<br />

-2.0<br />

190.0<br />

-2.0<br />

180.0<br />

-2.0<br />

381.0<br />

21.0<br />

24900.0<br />

120.0<br />

30.0<br />

71.0<br />

48.0<br />

22.0<br />

47.0<br />

-2.0<br />

200.0<br />

120.0<br />

39.0<br />

19.0<br />

39.0<br />

95.0<br />

-2.0<br />

47.0<br />

14.0<br />

218.0<br />

34.0<br />

-10.0<br />

100.0<br />

-19.0<br />

130.0<br />

64.0<br />

-19.0<br />

58.0<br />

93.0<br />

52.0<br />

95.0<br />

31.0<br />

997.0<br />

7.0<br />

2210.0<br />

343.0<br />

929.0<br />

140,0<br />

130.0<br />

82,0<br />

-18.0<br />

100.0<br />

97.0<br />

5.0<br />

50.0<br />

100.0<br />

OVERBURDEN DRILLING<br />

>>> H M C *C^<br />

Cu<br />

145.0<br />

155.0<br />

134.0<br />

54.0<br />

110.0<br />

48.0<br />

113.0<br />

48.0<br />

187.0<br />

72.0<br />

134,0<br />

132.0<br />

160.0<br />

184.0<br />

118.0<br />

125.0<br />

81.0<br />

93.0<br />

110.0<br />

43.0<br />

97.0<br />

96.0<br />

96.0<br />

98.0<br />

86.0<br />

32,0<br />

45.0<br />

7.0<br />

19.0<br />

13.0<br />

11.0<br />

9.0<br />

52.0<br />

56.0<br />

61.0<br />

22.0<br />

69.0<br />

70.0<br />

51.0<br />

65.0<br />

97.0<br />

64.0<br />

99.0<br />

25.0<br />

113.0<br />

98.0<br />

9.0<br />

9.0<br />

133.0<br />

141.0<br />

190.0<br />

132.0<br />

500.0<br />

36.0<br />

37.0<br />

16.0<br />

As<br />

17.0<br />

25.0<br />

22.0<br />

-0.5<br />

17.0<br />

1.1<br />

42.0<br />

-0.5<br />

18.0<br />

-0.5<br />

16.0<br />

23.0<br />

36.0<br />

29.0<br />

12.0<br />

16.0<br />

14.0<br />

7.8<br />

17.0<br />

1.4<br />

11.0<br />

8.5<br />

14.0<br />

10.0<br />

16.0<br />

5.3<br />

-0.5<br />

- .8<br />

- .8<br />

- .3<br />

- .7<br />

- .6<br />

12.0<br />

-8.9<br />

-8.0<br />

-8.1<br />

-8.7<br />

9.3<br />

11.0<br />

19.0<br />

12.0<br />

-9.1<br />

30.0<br />

-0.5<br />

23.0<br />

-10.0<br />

-9.8<br />

-9.5<br />

17.0<br />

27.0<br />

17.0<br />

21.0<br />

55.4<br />

1.6<br />

-8.6<br />

-8.9<br />

Sb<br />

0.5<br />

0.7<br />

0.6<br />

-0.1<br />

0.5<br />

0.1<br />

1.0<br />

-0.1<br />

0.4<br />

-0.1<br />

0.6<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.8<br />

0.5<br />

0.4<br />

0.4<br />

0.2<br />

0.4<br />

0.3<br />

0.5<br />

0.3<br />

0.5<br />

0.4<br />

-0.1<br />

0.5<br />

0.4<br />

0.4<br />

0.3<br />

0.5<br />

0.5<br />

-0.3<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

-0.2<br />

0.6<br />

0.5<br />

0.4<br />

0.8<br />

-0.1<br />

0.7<br />

0.3<br />

0.5<br />

0.4<br />

0.6<br />

0.5<br />

-0.3<br />

0.4<br />

0.6<br />

0.1<br />

0.4<br />

-0.3<br />

Ba<br />

-50.0<br />

-50.0<br />

-50.0<br />

770.0<br />

-50.0<br />

590.0<br />

-50.0<br />

720.0<br />

130.0<br />

1400.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

780.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

560.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-170.0<br />

-150.0<br />

-150.0<br />

-160.0<br />

-150.0<br />

-140.0<br />

-140.0<br />

-150.0<br />

-170.0<br />

-180.0<br />

650.0<br />

-160.0<br />

-180,0<br />

-170.0<br />

-170.0<br />

-160.0<br />

-150.0<br />

-170.0<br />

-160.0<br />

-170.0<br />

640.0<br />

-150.0<br />

-150.0<br />

Cd<br />

-13.0<br />

-15.0<br />

-14.0<br />

-5.0<br />

-13.0<br />

-5.0<br />

-13.0<br />

-5.0<br />

-14.0<br />

-5.0<br />

-15.0<br />

-14.0<br />

-16.0<br />

-14.0<br />

-13.0<br />

-12.0<br />

-14.0<br />

-13.0<br />

-13.0<br />

. -5.0<br />

-13.0<br />

-13.0<br />

-12.0<br />

-14.0<br />

-17.0<br />

-15.0<br />

-5.0<br />

-17.0<br />

-17.0<br />

-16.0<br />

-17.0<br />

-17.0<br />

-19.0<br />

-30.0<br />

-27.0<br />

-28.0<br />

-29.0<br />

-27.0<br />

-26.0<br />

-25.0<br />

-28.0<br />

-31.0<br />

-33.0<br />

-5.0<br />

-31.0<br />

-34.0<br />

-33.0<br />

-31.0<br />

-28.0<br />

-28.0<br />

-33.0<br />

-29.0<br />

-32.0<br />

-5.0<br />

-28.0<br />

-29.0<br />

Cs<br />

-0.5<br />

-0.5<br />

-0.5<br />

6.4<br />

-0.5<br />

4.3<br />

-0.5<br />

3.4<br />

-0.5<br />

7.5<br />

1.4<br />

-0.5<br />

-1.0<br />

-0.5<br />

0.9<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

4.3<br />

-0.5<br />

-0.5<br />

-0.5<br />

-0.5<br />

-1.0<br />

-0.5<br />

2.3<br />

-1.0<br />

-1.1<br />

1.8<br />

1.1<br />

-1.0<br />

-l.l<br />

-1.7<br />

-1.6<br />

-1.6<br />

-1.7<br />

1.7<br />

-1.4<br />

-1.5<br />

-1.6<br />

-1.8<br />

-1.9<br />

0.7<br />

2.3<br />

-1.9<br />

-1.9<br />

-1.9<br />

-1.7<br />

-1.6<br />

-1.9<br />

-1.6<br />

-1.8<br />

1.8<br />

-1.6<br />

-1.6<br />

Cr<br />

780.0<br />

B50.0<br />

820.0<br />

280.0<br />

730.0<br />

330.0<br />

700.0<br />

280.0<br />

740.0<br />

390.0<br />

640.0<br />

630.0<br />

760.0<br />

790.0<br />

690.0<br />

800.0<br />

700.0<br />

800.0<br />

720.0<br />

360.0<br />

730.0<br />

790.0<br />

640.0<br />

600.0<br />

750.0<br />

640.0<br />

230.0<br />

660.0<br />

840.0<br />

820.0<br />

740.0<br />

590.0<br />

790.0<br />

680.0<br />

700.0<br />

740.0<br />

750.0<br />

710.0<br />

690.0<br />

670.0<br />

820.0<br />

780.0<br />

860.0<br />

400.0<br />

870.0<br />

870.0<br />

1000.0<br />

1000.0<br />

860.0<br />

850.0<br />

970.0<br />

740.0<br />

660.0<br />

360.0<br />

740.0<br />

860.0<br />

Co<br />

120.0<br />

150.0<br />

130.0<br />

26.0<br />

120.0<br />

33.0<br />

120.0<br />

33.0<br />

150.0<br />

39.0<br />

130.0<br />

120.0<br />

180.0<br />

190.0<br />

110.0<br />

120.0<br />

85.0<br />

90.0<br />

110.0<br />

32.0<br />

110.0<br />

98.0<br />

95.0<br />

85.0<br />

100.0<br />

43.0<br />

22.0<br />

30.0<br />

28.0<br />

40.0<br />

34.0<br />

33.0<br />

73.0<br />

57.0<br />

63.0<br />

54.0<br />

69.0<br />

77.0<br />

63.0<br />

66.0<br />

88.0<br />

90.0<br />

110.0<br />

25.0<br />

120.0<br />

89.0<br />

30.0<br />

36.0<br />

140.0<br />

140.0<br />

160.0<br />

130.0<br />

290.0<br />

22.0<br />

54.0<br />

39.0<br />

[87/12/22]<br />

Eu<br />

9.0<br />

e.o<br />

7.0<br />

1.0<br />

9.0<br />

2.0<br />

6.0<br />

2.0<br />

8.0<br />

2.0<br />

7.0<br />

7.0<br />

7.0<br />

6.0<br />

9.0<br />

6.0<br />

8.0<br />

9.0<br />

7.0<br />

-1.0<br />

8.0<br />

10.0<br />

11.0<br />

9.0<br />

9.0<br />

7.0<br />

2.0<br />

9.0<br />

7.0<br />

9.0<br />

8.0<br />

6.0<br />

9.0<br />

8.0<br />

e.o<br />

e.o<br />

7.0<br />

8.0<br />

9.0<br />

9.0<br />

7.0<br />

9.0<br />

7.0<br />

-1.0<br />

10.0<br />

8.0<br />

5.0<br />

6.0<br />

7.0<br />

7.0<br />

7.0<br />

6.0<br />

e.o<br />

-1.0<br />

7.0<br />

7.0<br />

Hf<br />

273.0<br />

242.0<br />

281.0<br />

4.0<br />

226.0<br />

4.0<br />

241.0<br />

4.0<br />

222.0<br />

4.0<br />

229.0<br />

219.0<br />

206.0<br />

195.0<br />

255.0<br />

98.0<br />

294.0<br />

122.0<br />

223.0<br />

5.0<br />

210.0<br />

160.0<br />

300.0<br />

293.0<br />

296.0<br />

156.0<br />

4.0<br />

360.0<br />

293.0<br />

270.0<br />

347.0<br />

369.0<br />

357.0<br />

331.0<br />

334.0<br />

330.0<br />

362.0<br />

397.0<br />

357.0<br />

324.0<br />

325.0<br />

228.0<br />

246.0<br />

5.0<br />

275.0<br />

213.0<br />

182.0<br />

153.0<br />

209.0<br />

208.0<br />

221.0<br />

234.0<br />

146.0<br />

4.0<br />

218.0<br />

278.0<br />

Ir<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-50.0<br />

-100.0<br />

-110.0<br />

-50.0<br />

-50.0<br />

-110.0<br />

-110.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-100.0<br />

-50.0<br />

-100.0<br />

-50.0<br />

-50.0<br />

-50.0


l l l l<br />

l<br />

l<br />

l<br />

l l<br />

l l<br />

l l l<br />

l l<br />

l l<br />

l<br />

fiecor Hole Saip tp<br />

1120<br />

1121<br />

127<br />

127<br />

1122 127<br />

1123 127<br />

1124 127<br />

1125 127<br />

1126 127<br />

1127 127<br />

1128 127<br />

1129 127<br />

1130 127<br />

1131 127<br />

1132 127<br />

1133 127<br />

1134 127<br />

1135 127<br />

1136 127<br />

1137 127<br />

1138 127<br />

1139 126<br />

1140 128<br />

1141 128<br />

1142 128<br />

1143 128<br />

1144 128<br />

1145 128<br />

1146 128<br />

1147 128<br />

1148 128<br />

1149 128<br />

1150 128<br />

1151 128<br />

1152 128<br />

1153 128<br />

1154 128<br />

1155 128<br />

1156 129<br />

1157 129<br />

1158 129<br />

1159 129<br />

1160 129<br />

1161 129<br />

1162 129<br />

1163 129<br />

1164 129<br />

1165 129<br />

1166 129<br />

1167 130<br />

1168 130<br />

1169 130<br />

1170 130<br />

1171 130<br />

1172 130<br />

1173 130<br />

1174 130<br />

1175 130<br />

RNTBUSH OVERBURDEN DRILLI NG >>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Recor Hole Saip<br />

1176 130<br />

1177 130<br />

1178 131<br />

1179 131<br />

1180 131<br />

1181 131<br />

1182 131<br />

1183 131<br />

1184 131<br />

1185 131<br />

1186 131<br />

1187 132<br />

1188 132<br />

11B9 132<br />

1190 132<br />

1191 132<br />

1192 132<br />

1193 132<br />

1194 132<br />

1195 132<br />

1196 133<br />

1197 133<br />

RNTBUSH OVERBURDEN DRILLING<br />

>>> H<br />

up<br />

10<br />

11 12 3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

1<br />

2<br />

Au<br />

94.0<br />

-2.0<br />

537.0<br />

-21.0<br />

61.0<br />

58.0<br />

50.0<br />

-40.0<br />

-19.0<br />

-2.0<br />

-5.0<br />

27.0<br />

378.0<br />

160.0<br />

66.0<br />

1420.0<br />

39.0<br />

59.0<br />

-2.0<br />

-2.0<br />

120.0<br />

-2.0<br />

Cu<br />

188.0<br />

43.0<br />

9.0<br />

38.0<br />

68.0<br />

132.0<br />

42.0<br />

37.0<br />

78.0<br />

100.0<br />

46.0<br />

21.0<br />

85.0<br />

72.0<br />

91.0<br />

76.0<br />

82.0<br />

66.0<br />

42.0<br />

53.0<br />

94.0<br />

70.0<br />

As<br />

77.4<br />

0.9<br />

-12.0<br />

-12.0<br />

-12.0<br />

-13.0<br />

-10.0<br />

-22.0<br />

62.0<br />

-0.5<br />

-0.5<br />

-9.1<br />

-8.4<br />

-12.0<br />

-12.0<br />

15.0<br />

13.0<br />

-12.0<br />

-0.5<br />

1.0<br />

10.0<br />

-0.5<br />

Sb<br />

0.5<br />

-0.1<br />

-0.3<br />

0.7<br />

0.3<br />

0.6<br />

0.6<br />

-0.6<br />

1.0<br />

-0.1<br />

-0.1<br />

0.4<br />

0.5<br />

-0.3<br />

-0.3<br />

0.4<br />

0.5<br />

-0.3<br />

-0.1<br />

-0.1<br />

0.5<br />

-0.1<br />

Ba<br />

-140.0<br />

680.0<br />

-160.0<br />

-170.0<br />

-170.0<br />

-170.0<br />

-120.0<br />

-300.0<br />

-160.0<br />

280.0<br />

240.0<br />

-120.0<br />

-110.0<br />

-150.0<br />

-150.0<br />

-140.0<br />

-150.0<br />

-150.0<br />

160.0<br />

110.0<br />

-50.0<br />

-50.0<br />

Cd<br />

-29.0<br />

-5.0<br />

-33.0<br />

-34.0<br />

-35.0<br />

-38.0<br />

-30.0<br />

-65.0<br />

-34.0<br />

-5.0<br />

-5.0<br />

-26.0<br />

-24.0<br />

-32.0<br />

-33.0<br />

-33.0<br />

-33.0<br />

-32.0<br />

-5.0<br />

-5.0<br />

-20.0<br />

-5.0<br />

Cs<br />

-1.5<br />

2.0<br />

-1.7<br />

-1.7<br />

-1.7<br />

-1.8<br />

-1.4<br />

-3.8<br />

-1.6<br />

2.4<br />

3.0<br />

1.4<br />

-1.1<br />

-1.6<br />

-1.6<br />

-1.6<br />

-1.6<br />

-1.6<br />

1.2<br />

1.4<br />

-0.5<br />

0.9<br />

M<br />

C<br />

Cr<br />

770.0<br />

240.0<br />

950.0<br />

790.0<br />

840.0<br />

620.0<br />

700.0<br />

780.0<br />

900.0<br />

210.0<br />

240.0<br />

890.0<br />

870.0<br />

810.0<br />

810.0<br />

830.0<br />

920.0<br />

7BO.O<br />

140.0<br />

110.0<br />

780.0<br />

270.0<br />


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

Recor<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

23<br />

24<br />

25<br />

26<br />

27<br />

28<br />

29<br />

30<br />

31<br />

32<br />

33<br />

34<br />

35<br />

36<br />

37<br />

38<br />

39<br />

40<br />

41<br />

42<br />

43<br />

44<br />

45<br />

46<br />

47<br />

4B<br />

49<br />

50<br />

51<br />

52<br />

53<br />

54<br />

55<br />

56<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

1<br />

2<br />

2<br />

2 22 2<br />

2<br />

2<br />

2<br />

2<br />

2<br />

3<br />

3<br />

3<br />

3<br />

3<br />

3<br />

3<br />

3<br />

4<br />

4<br />

4<br />

4<br />

4<br />

5<br />

5<br />

5<br />

5<br />

5<br />

5<br />

5<br />

6<br />

6<br />

6<br />

7<br />

7<br />

7<br />

7<br />

7<br />

7<br />

7<br />

7<br />

8<br />

B<br />

8<br />

9<br />

Hole<br />

RNTBUSH OVERBURDEN DRILL<br />

up<br />

i<br />

2<br />

3<br />

4<br />

5<br />

b<br />

7<br />

8<br />

9<br />

10<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

e<br />

9<br />

10<br />

11<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

3<br />

4<br />

5<br />

t,<br />

1<br />

1<br />

l<br />

3<br />

i<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

1<br />

fei<br />

16.0<br />

18.0<br />

20.4<br />

20.0.<br />

21.2<br />

22.6<br />

21.2<br />

21.5<br />

20.0<br />

4.6<br />

18.0<br />

20.0<br />

20.5<br />

21.5<br />

17.0<br />

20.3<br />

21.4<br />

28.0<br />

24.5<br />

26.2<br />

4.6<br />

20.0<br />

20.8<br />

20.0<br />

22.3<br />

20.0<br />

22.4<br />

21.5<br />

4.7<br />

25.5<br />

22.2<br />

24.6<br />

20.5<br />

5.3<br />

22.8<br />

23.2<br />

20.2<br />

20.0<br />

21.1<br />

20.0<br />

5.0<br />

24.2<br />

22.7<br />

5.4<br />

17.0<br />

19.0<br />

20.9<br />

20.1<br />

23.4<br />

22.1<br />

21.7<br />

4.6<br />

18.0<br />

19.0<br />

4.9<br />

20.6<br />

La<br />

291.0<br />

311.0<br />

333.0<br />

302.0<br />

253.0<br />

310.0<br />

342.0<br />

384.0<br />

294.0<br />

22.0<br />

309.0<br />

295.0<br />

313.0<br />

365.0<br />

260.0<br />

310.0<br />

334.0<br />

399.0<br />

382.0<br />

431.0<br />

29.0<br />

388.0<br />

408.0<br />

381.0<br />

352.0<br />

316,0<br />

296.0<br />

295.0<br />

30.0<br />

443.0<br />

682.0<br />

818.0<br />

731.0<br />

30.0<br />

340.0<br />

327.0<br />

342.0<br />

301.0<br />

281.0<br />

306.0<br />

22.0<br />

349.0<br />

274.0<br />

29.0<br />

374,0<br />

416.0<br />

385.0<br />

336.0<br />

369.0<br />

201.0<br />

275.0<br />

30.0<br />

379.0<br />

332,0<br />

31.0<br />

328.0<br />

Ho<br />

-1.0<br />

3.0<br />

3.0<br />

5.0<br />

10.0<br />

19.0<br />

8.0<br />

6.0<br />

10.0<br />

1.0<br />

3.0<br />

1.0<br />

4.0<br />

30.0<br />

7.0<br />

4.0<br />

4.0<br />

6.0<br />

5.0<br />

5.0<br />

3.0<br />

1.0<br />

4.0<br />

4.0<br />

5.0<br />

3.0<br />

4.0<br />

6.0<br />

2.0<br />

7.0<br />

2.0<br />

3.0<br />

2.0<br />

1.0<br />

5.0<br />

5.0<br />

4.0<br />

5.0<br />

7.0<br />

5.0<br />

2.0<br />

5.0<br />

6.0<br />

2.0<br />

3.0<br />

2.0<br />

4.0<br />

3.0<br />

4.0<br />

7.0<br />

9.0<br />

2.0<br />

3.0<br />

3.0<br />

3.0<br />

2,0<br />

Ni<br />

-20.0<br />

41.0<br />

76.0<br />

42.0<br />

160.0<br />

95.0<br />

67.0<br />

160.0<br />

110.0<br />

70.0<br />

34.0<br />

78.0<br />

94.0<br />

97.0<br />

63.0<br />

110.0<br />

93.0<br />

140.0<br />

150.0<br />

150.0<br />

B3.0<br />

-20.0<br />

-20.0<br />

24.0<br />

110.0<br />

64.0<br />

390.0<br />

210.0<br />

70.0<br />

140.0<br />

63.0<br />

120.0<br />

45.0<br />

99.0<br />

100.0<br />

110.0<br />

85.0<br />

110.0<br />

130.0<br />

91.0<br />

72.0<br />

160.0<br />

220.0<br />

77.0<br />

-20.0<br />

24.0<br />

72.0<br />

96.0<br />

160.0<br />

290.0<br />

170.0<br />

65.0<br />

88.0<br />

280.0<br />

68,0<br />

90.0<br />

Rb<br />

10.0<br />

12.0<br />

10.0<br />

7.0<br />

13.0<br />

12.0<br />

-5.0<br />

15.0<br />

-5.0<br />

99.0<br />

8.0<br />

10.0<br />

10.0<br />

-5.0<br />

-5.0<br />

10.0<br />

-5.0<br />

15.0<br />

9.0<br />

12.0<br />

97.0<br />

-5.0<br />

-5.0<br />

13.0<br />

13.0<br />

-5.0<br />

-5.0<br />

15.0<br />

110.0<br />

9.0<br />

-11.0<br />

-12.0<br />

19.0<br />

100.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

11.0<br />

10.0<br />

-5.0<br />

110.0<br />

12.0<br />

11.0<br />

BO.O<br />

15.0<br />

-5,0<br />

-5.0<br />

12.0<br />

-5.0<br />

-5.0<br />

8.0<br />

97.0<br />

10.0<br />

-5.0<br />

84.0<br />

9.0<br />

ING<br />

Se<br />

68.0<br />

78.6<br />

85.3<br />

62.0<br />

77.9<br />

74.9<br />

80.0<br />

82. 1<br />

76.2<br />

13.0<br />

79.2<br />

77.0<br />

74.8<br />

73.2<br />

75.2<br />

74.7<br />

76.7<br />

82.3<br />

80.1<br />

90.1<br />

14.0<br />

73.fl<br />

81.9<br />

79.2<br />

76.4<br />

72.0<br />

62.0<br />

74.0<br />

15.0<br />

75.0<br />

79.4<br />

79.1<br />

77.0<br />

16.0<br />

79.2<br />

76.0<br />

74.9<br />

67.5<br />

70.9<br />

B0.2<br />

16.0<br />

62.1<br />

58.4<br />

19.0<br />

74.5<br />

80.7<br />

76.6<br />

68.6<br />

71.3<br />

57.9<br />

62.3<br />

14.0<br />

78.4<br />

74.0<br />

16.0<br />

72.9<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

2 of<br />

Recor Hole Satp<br />

57 9<br />

58<br />

59<br />

60<br />

61<br />

62<br />

63<br />

64<br />

65<br />

66<br />

67 10<br />

68 10<br />

69 10<br />

70 10<br />

71 10<br />

72 11<br />

73 11<br />

74 12<br />

75 12<br />

76 12<br />

77 12<br />

78 12<br />

79 12<br />

80 12<br />

Bl 12<br />

82 12<br />

83 12<br />

84 12<br />

85 12<br />

86 12<br />

B7 12<br />

88 12<br />

89 12<br />

90 12<br />

91 12<br />

92 12<br />

93 12<br />

94 13<br />

95 13<br />

96 13<br />

97 13<br />

98 14<br />

99 14<br />

100 14<br />

101 15<br />

102 15<br />

103 16<br />

104 16<br />

105 16<br />

106 16<br />

107 16<br />

108 16<br />

109 16<br />

110 17<br />

111 17<br />

112 17<br />

RNTBUSH OVERBURDEN DRILLING<br />

tip<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

li<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

FeX<br />

21.5<br />

19.0<br />

19.0<br />

19.0<br />

20.0<br />

21.2<br />

21.3<br />

21.9<br />

18.0<br />

5.3<br />

21.7<br />

22.9<br />

21.8<br />

22.5<br />

4.9<br />

23.4<br />

5.4<br />

24.5<br />

21.9<br />

22.9<br />

20.9<br />

23.5<br />

23.9<br />

22.0<br />

21.0<br />

25.2<br />

23.9<br />

17.0<br />

27.0<br />

24.3<br />

25.9<br />

28.5<br />

24.6<br />

24.0<br />

24.6<br />

25.7<br />

4.8<br />

22.2<br />

23.8<br />

23.8<br />

4.7<br />

23.5<br />

22.3<br />

4.9<br />

24.9<br />

5.0<br />

21.5<br />

20.5<br />

20.5<br />

24.7<br />

21.6<br />

23.0<br />

3.8<br />

20.9<br />

21.6<br />

24.1<br />

Li<br />

355.0<br />

341.0<br />

322.0<br />

286.0<br />

289,0<br />

292.0<br />

346.0<br />

325.0<br />

289.0<br />

31.0<br />

372.0<br />

393.0<br />

373.0<br />

437.0<br />

57.0<br />

418.0<br />

33.0<br />

374.0<br />

388.0<br />

395.0<br />

354.0<br />

430.0<br />

471.0<br />

423.0<br />

329.0<br />

617.0<br />

518.0<br />

470.0<br />

751.0<br />

761.0<br />

818.0<br />

1260.0<br />

976.0<br />

820.0<br />

513.0<br />

472.0<br />

21.0<br />

485.0<br />

456.0<br />

403.0<br />

31.0<br />

480.0<br />

455.0<br />

30.0<br />

382.0<br />

36.0<br />

433.0<br />

464.0<br />

480.0<br />

489.0<br />

412.0<br />

597.0<br />

24.0<br />

382.0<br />

343.0<br />

409.0<br />

Mo<br />

-1.0<br />

4.0<br />

2.0<br />

4.0<br />

3.0<br />

3.0<br />

34.0<br />

3.0<br />

5.0<br />

2.0<br />

2.0<br />

1.0<br />

2.0<br />

2.0<br />

5.0<br />

3.0<br />

2.0<br />

3.0<br />

-2.0<br />

-1.0<br />

-1.0<br />

-1.0<br />

3.0<br />

4.0<br />

1.0<br />

-1.0<br />

4.0<br />

2.0<br />

-3.0<br />

-3.0<br />

-4.0<br />

-4.0<br />

-4.0<br />

24.0<br />

-3.0<br />

-3.0<br />

1.0<br />

2.0<br />

3.0<br />

1.0<br />

3.0<br />

-1.0<br />

-1.0<br />

3.0<br />

-1.0<br />

2.0<br />

-1.0<br />

1.0<br />

-1.0<br />

-1.0<br />

-2.0<br />

-3.0<br />

1.0<br />

3.0<br />

-1.0<br />

-1.0<br />

Hi<br />

110.0<br />

79.0<br />

78.0<br />

98.0<br />

100.0<br />

110.0<br />

87.0<br />

100.0<br />

89.0<br />

84.0<br />

86.0<br />

120.0<br />

78.0<br />

77.0<br />

160.0<br />

120.0<br />

96.0<br />

70.0<br />

140.0<br />

9B.O<br />

80.0<br />

67.0<br />

110.0<br />

65.0<br />

93.0<br />

45.0<br />

80.0<br />

74.0<br />

42.0<br />

58.0<br />

-39.0<br />

-41.0<br />

-34.0<br />

60.0<br />

43.0<br />

76.0<br />

44.0<br />

140.0<br />

110.0<br />

140.0<br />

79.0<br />

84.0<br />

130.0<br />

71.0<br />

150.0<br />

89.0<br />

92.0<br />

66.0<br />

80.0<br />

87.0<br />

120.0<br />

65.0<br />

74.0<br />

66.0<br />

42.0<br />

29.0<br />

Rb<br />

-5.0<br />

7.0<br />

-5.0<br />

B.O<br />

10.0<br />

9.0<br />

8.0<br />

10.0<br />

10.0<br />

65.0<br />

-5.0<br />

-17.0<br />

-15.0<br />

-15.0<br />

52.0<br />

-15.0<br />

110.0<br />

-15.0<br />

-13.0<br />

-13.0<br />

19.0<br />

-15.0<br />

-16.0<br />

-15.0<br />

-12.0<br />

-23.0<br />

-14.0<br />

16.0<br />

-19.0<br />

-18.0<br />

-22.0<br />

-24.0<br />

-20.0<br />

26.0<br />

-15.0<br />

-21.0<br />

70.0<br />

-16.0<br />

-17.0<br />

22.0<br />

87.0<br />

-15.0<br />

-15.0<br />

75.0<br />

18.0<br />

130.0<br />

-13.0<br />

-14.0<br />

-14.0<br />

-16.0<br />

-13.0<br />

-14.0<br />

80.0<br />

-15.0<br />

18.0<br />

-15.0<br />

Se<br />

77.0<br />

73.0<br />

70.2<br />

71.2<br />

73.0<br />

73.3<br />

75.3<br />

71.2<br />

70.9<br />

16.0<br />

75.4<br />

75.1<br />

76.3<br />

81.1<br />

14.0<br />

77.6<br />

17.0<br />

74.4<br />

73.0<br />

77.7<br />

79.4<br />

84.8<br />

85.1<br />

B7.7<br />

77.6<br />

B5.2<br />

87.1<br />

70.5<br />

91.2<br />

94.5<br />

100.0<br />

9B.9<br />

88.1<br />

101.0<br />

103.0<br />

120.0<br />

15.0<br />

B8.9<br />

96.4<br />

88.0<br />

16.0<br />

90.1<br />

89.1<br />

14.0<br />

89.1<br />

18.0<br />

90.9<br />

93.6<br />

92.4<br />

97.1<br />

88.3<br />

100.0<br />

11.0<br />

99.4<br />

90.2<br />

94.5<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

3 of<br />

Recor Hole Saip<br />

113 17<br />

114 17<br />

115 17<br />

116 17<br />

117 17<br />

118 17<br />

119 17<br />

120 17<br />

121 17<br />

122 17<br />

123 17<br />

124 17<br />

125 17<br />

126 17<br />

127 17<br />

128 17<br />

129 17<br />

130 17<br />

131 18<br />

132 18<br />

133 18<br />

134 18<br />

135 IB<br />

136 18<br />

137 19<br />

138 19<br />

139 19<br />

140 19<br />

141 19<br />

142 19<br />

143 19<br />

144 20<br />

145 20<br />

146 20<br />

147 20<br />

148 20<br />

149 20<br />

150 20<br />

151 20<br />

152 20<br />

153 20<br />

154 20<br />

155 20<br />

156 20<br />

157 20<br />

158 20<br />

159 20<br />

160 21<br />

161 21<br />

162 21<br />

163 21<br />

164 21<br />

165 21<br />

166 21<br />

167 21<br />

166 21<br />

RNTBUSH OVERBURDEN DRILL<br />

up<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

S<br />

9<br />

fei<br />

20.4<br />

20.0<br />

21.7<br />

19.0<br />

21.4<br />

20.0<br />

23.6<br />

23.4<br />

22.9<br />

21.7<br />

24.2<br />

27.3<br />

26.7<br />

23.4<br />

24.2<br />

22.9<br />

21.7<br />

3.9<br />

26.3<br />

25.2<br />

22.8<br />

22.7<br />

21.0<br />

4.4<br />

24.9<br />

24.4<br />

23.9<br />

20.6'<br />

20.5-<br />

22.1<br />

5.3<br />

23.2<br />

23.6<br />

22.1<br />

22.8<br />

27.0<br />

21,3<br />

22.9<br />

20.7<br />

21.3<br />

19.0<br />

22.5<br />

21.5<br />

19.0<br />

17.0<br />

20.8<br />

4.4<br />

16.0<br />

17.0<br />

18.0<br />

19.0<br />

20.0<br />

19.0<br />

19.0<br />

17.0<br />

19.0<br />

La<br />

329.0<br />

288.0<br />

354.0<br />

340.0<br />

372.0<br />

332.0<br />

364.0<br />

416.0<br />

395.0<br />

393.0<br />

422.0<br />

240.0<br />

363.0<br />

512.0<br />

501.0<br />

556.0<br />

465.0<br />

22.0<br />

421.0<br />

438.0<br />

470.0<br />

886.0<br />

546.0<br />

49.0<br />

443.0<br />

436.0<br />

348.0<br />

558.0<br />

458.0<br />

480.0<br />

29.0<br />

369.0<br />

368.0<br />

366.0<br />

426.0<br />

482.0<br />

411.0<br />

416.0<br />

362.0<br />

413.0<br />

334.0<br />

425.0<br />

587.0<br />

546.0<br />

435.0<br />

495.0<br />

28.0<br />

436.0<br />

451.0<br />

378.0<br />

345.0<br />

363.0<br />

346.0<br />

311.0<br />

283.0<br />

376.0<br />

Ko<br />

3.0<br />

1.0<br />

4.0<br />

3.0<br />

6.0<br />

3.0<br />

4.0<br />

7.0<br />

5.0<br />

8.0<br />

7.0<br />

3.0<br />

6.0<br />

4.0<br />

2.0<br />

6.0<br />

2.0<br />

3.0<br />

8.0<br />

3.0<br />

2.0<br />

-1.0<br />

3.0<br />

2.0<br />

-1.0<br />

2.0<br />

9.0<br />

2.0<br />

3.0<br />

-1.0<br />

2.0<br />

6.0<br />

6.0<br />

7.0<br />

-1.0<br />

5.0<br />

-1.0<br />

1.0<br />

5.0<br />

-1.0<br />

5.0<br />

5.0<br />

4.0<br />

-1.0<br />

2.0<br />

-3.0<br />

2.0<br />

2.0<br />

2.0<br />

4.0<br />

5.0<br />

6.0<br />

5.0<br />

8.0<br />

3.0<br />

5.0<br />

Hi<br />

85.0<br />

62.0<br />

110.0<br />

87.0<br />

95.0<br />

78.0<br />

120.0<br />

110.0<br />

82.0<br />

73.0<br />

94.0<br />

160.0<br />

130.0<br />

61.0<br />

92.0<br />

39.0<br />

160.0<br />

74.0<br />

160.0<br />

150.0<br />

88.0<br />

-35.0<br />

290.0<br />

45.0<br />

150.0<br />

150.0<br />

170.0<br />

-27.0<br />

37.0<br />

77.0<br />

86.0<br />

130.0<br />

160.0<br />

45.0<br />

59.0<br />

110.0<br />

110.0<br />

88.0<br />

80.0<br />

70,0<br />

46,0<br />

71.0<br />

33.0<br />

42.0<br />

68.0<br />

-27.0<br />

50.0<br />

33.0<br />

40.0<br />

100.0<br />

90.0<br />

72.0<br />

92.0<br />

110.0<br />

44.0<br />

51.0<br />

Rb<br />

-13.0<br />

-11.0<br />

-15.0<br />

-14.0<br />

-14.0<br />

-12.0<br />

-15.0<br />

-14.0<br />

-14.0<br />

-14.0<br />

-13.0<br />

14.0<br />

-14.0<br />

-17.0<br />

-15.0<br />

-20.0<br />

-16.0<br />

62.0<br />

-17.0<br />

-18.0<br />

19.0<br />

-20.0<br />

-18.0<br />

88.0<br />

-19.0<br />

-16.0<br />

-15.0<br />

-15.0<br />

-13.0<br />

-14.0<br />

92.0<br />

19.0<br />

-14.0<br />

-12.0<br />

-14.0<br />

-14.0<br />

14.0<br />

-13.0<br />

19.0<br />

-14.0<br />

-14.0<br />

-15.0<br />

19.0<br />

-14.0<br />

-12.0<br />

-15.0<br />

63.0<br />

-14.0<br />

-13.0<br />

-14.0<br />

-14.0<br />

18.0<br />

-13.0<br />

-17.0<br />

-13.0<br />

-13.0<br />

IN6<br />

Se<br />

71.0<br />

72.1<br />

75.2<br />

71.6<br />

79.7<br />

74.3<br />

88.7<br />

80.2<br />

81.7<br />

81.8<br />

80.3<br />

63.1<br />

89,1<br />

91.3<br />

91.6<br />

91.8<br />

81.4<br />

12.0<br />

81.8<br />

92.8<br />

86.1<br />

93.5<br />

70.2<br />

13.0<br />

80.8<br />

79.2<br />

77.7<br />

92.8<br />

B8.7<br />

89.3<br />

19.0<br />

81.4<br />

83.6<br />

84.2<br />

91.7<br />

95.4<br />

80.4<br />

81.3<br />

78.6<br />

88.9<br />

80.3<br />

84.7<br />

93.8<br />

81.0<br />

79.1<br />

61.0<br />

13.0<br />

77.5<br />

81.2<br />

79.7<br />

84.2<br />

84.5<br />

84.6<br />

60.5<br />

80.9<br />

62.1<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

4 of<br />

Recor Hole Saip<br />

169 21<br />

170 21<br />

171 21<br />

172 21<br />

173 21<br />

174 21<br />

175 21<br />

176 21<br />

177 21<br />

178 22<br />

179 22<br />

180 22<br />

181 22<br />

182 22<br />

183 23<br />

184 23<br />

185 23<br />

186 23<br />

187 23<br />

188 23<br />

189 23<br />

190 23<br />

191 23<br />

192 23<br />

193 23<br />

194 23<br />

195 23<br />

196 24<br />

197 24<br />

198 24<br />

199 24<br />

200 24<br />

201 24<br />

202 24<br />

203 24<br />

204 24<br />

205 24<br />

206 24<br />

207 24<br />

208 24<br />

209 24<br />

210 24<br />

211 24<br />

212 24<br />

213 24<br />

214 25<br />

215 25<br />

216 25<br />

217 25<br />

218 25<br />

219 25<br />

220 25<br />

221 25<br />

222 25<br />

223 25<br />

224 25<br />

RNTBUSH OVERBURDEN DRILL<br />

up<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

FeU<br />

20.0<br />

21.5<br />

23.7<br />

20.8<br />

20.3<br />

24.8<br />

20.2<br />

22.3<br />

5.1<br />

20.3<br />

19.0<br />

17.0<br />

18.0<br />

4.7<br />

20.0<br />

21.2<br />

23.0<br />

22.6<br />

22.5<br />

21.6<br />

24.5<br />

23.2<br />

24.9<br />

24.3<br />

25.7<br />

20.9<br />

5.5<br />

20.7<br />

20.8<br />

20.0<br />

22.7<br />

22.3<br />

22.1<br />

21.1<br />

22.0<br />

22.7<br />

22.9<br />

21.6<br />

22.1<br />

23.3<br />

23.8<br />

20.3<br />

20.7<br />

23.0<br />

6.1<br />

21.0<br />

21.7<br />

22.1<br />

21.5<br />

22.9<br />

22.2<br />

24.6<br />

22.6<br />

22.2<br />

20.5<br />

20.9<br />

La<br />

377.0<br />

436.0<br />

503.0<br />

419.0<br />

617.0<br />

766.0<br />

1290.0<br />

658.0<br />

150.0<br />

568.0<br />

600.0<br />

464.0<br />

364.0<br />

31.0<br />

393.0<br />

356.0<br />

355.0<br />

390.0<br />

330.0<br />

328.0<br />

361.0<br />

332.0<br />

343.0<br />

416.0<br />

513.0<br />

597.0<br />

33.0<br />

261.0<br />

431.0<br />

448.0<br />

475.0<br />

421.0<br />

407.0<br />

405.0<br />

457.0<br />

466.0<br />

482.0<br />

461.0<br />

464.0<br />

520.0<br />

452.0<br />

426.0<br />

715.0<br />

578.0<br />

16.0<br />

501.0<br />

579.0<br />

461.0<br />

423.0<br />

483,0<br />

463.0<br />

499.0<br />

500.0<br />

421.0<br />

455.0<br />

378.0<br />

Ho<br />

4.0<br />

5.0<br />

6.0<br />

4.0<br />

6.0<br />

2,0<br />

-4.0<br />

3.0<br />

2.0<br />

-1.0<br />

6.0<br />

-1.0<br />

5.0<br />

1.0<br />

6.0<br />

4.0<br />

7.0<br />

4.0<br />

5.0<br />

6.0<br />

5.0<br />

7.0<br />

11.0<br />

4.0<br />

4.0<br />

7.0<br />

2.0<br />

3.0<br />

6.0<br />

6.0<br />

4.0<br />

3.0<br />

7.0<br />

2.0<br />

7.0<br />

7.0<br />

3.0<br />

5.0<br />

i.O<br />

6.0<br />

10.0<br />

7.0<br />

9.0<br />

4.0<br />

-1.0<br />

3.0<br />

5.0<br />

7.0<br />

4.0<br />

5.0<br />

6.0<br />

3.0<br />

7.0<br />

5.0<br />

120.0<br />

3.0<br />

Hi<br />

67.0<br />

100.0<br />

65.0<br />

72.0<br />

-32.0<br />

-32.0<br />

-41.0<br />

-32.0<br />

57.0<br />

49.0<br />

-32.0<br />

48.0<br />

70.0<br />

68.0<br />

83.0<br />

84.0<br />

160.0<br />

110.0<br />

130.0<br />

98.0<br />

120.0<br />

140.0<br />

150.0<br />

120.0<br />

120.0<br />

110.0<br />

80.0<br />

46.0<br />

-31.0<br />

41.0<br />

47.0<br />

100.0<br />

95.0<br />

120.0<br />

160.0<br />

88.0<br />

91.0<br />

110.0<br />

80.0<br />

71.0<br />

110.0<br />

60.0<br />

62.0<br />

73.0<br />

380.0<br />

51.0<br />

38.0<br />

83.0<br />

120.0<br />

140.0<br />

120.0<br />

130.0<br />

170.0<br />

130.0<br />

130,0<br />

110.0<br />

Rb<br />

-13.0<br />

-15.0<br />

-19.0<br />

-15.0<br />

-18.0<br />

-18.0<br />

-25.0<br />

-18.0<br />

34.0<br />

-17.0<br />

-18.0<br />

22.0<br />

-14.0<br />

85.0<br />

18.0<br />

-13.0<br />

-15.0<br />

-15.0<br />

-15.0<br />

-14.0<br />

-18.0<br />

-16.0<br />

-15.0<br />

-16.0<br />

-17.0<br />

-17.0<br />

66.0<br />

-12.0<br />

-16.0<br />

-14.0<br />

-16.0<br />

21.0<br />

-22.0<br />

-16.0<br />

-16.0<br />

-16.0<br />

-15.0<br />

-13.0<br />

-13.0<br />

17.0<br />

-16.0<br />

-14.0<br />

-16.0<br />

13.0<br />

84.0<br />

-15.0<br />

-14.0<br />

25.0<br />

-13.0<br />

-14.0<br />

15.0<br />

-15.0<br />

-15.0<br />

-14.0<br />

17.0<br />

-12.0<br />

ING<br />

Se<br />

80.5<br />

85.0<br />

96.0<br />

65.8<br />

95.2<br />

102.0<br />

88.0<br />

113.0<br />

14.0<br />

93.4<br />

87.5<br />

71.7<br />

82.1<br />

15.0<br />

79.3<br />

B3.4<br />

83.3<br />

B2.8<br />

80.8<br />

83.9<br />

86.6<br />

84.7<br />

82.6<br />

88.9<br />

92.2<br />

75.8<br />

17.0<br />

93.0<br />

93.4<br />

91.4<br />

96.8<br />

90.4<br />

82.6<br />

80.1<br />

80.4<br />

89.6<br />

92.4<br />

90.7<br />

90.2<br />

96.4<br />

93.3<br />

92.6<br />

88.8<br />

87.8<br />

24.4<br />

100.0<br />

102.0<br />

94.2<br />

88.6<br />

90.2<br />

87.5<br />

91.8<br />

87.0<br />

93.1<br />

79.7<br />

84.6<br />

>>> H M c


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RIMTBUSH OVERBURDEN DRILLING<br />

:tp<br />

12<br />

13<br />

14<br />

15<br />

16<br />

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21.8<br />

22.5<br />

22.5<br />

22.9<br />

21.2<br />

24.8<br />

22.3<br />

6.0<br />

20.1<br />

21.3<br />

22.4<br />

19.0<br />

20.0<br />

21.7<br />

21.9<br />

23.8<br />

22.0<br />

21.8<br />

35.7<br />

23.7<br />

20.0<br />

20.9<br />

22.9<br />

21.3<br />

24.3<br />

20.8<br />

23.2<br />

20.0<br />

21.2<br />

20.2<br />

22.2<br />

4.8<br />

23.2<br />

20.4<br />

21.9<br />

24.5<br />

23.6<br />

22.2<br />

25.5<br />

24. B<br />

21.2<br />

22.6<br />

23.0<br />

24.2<br />

22.9<br />

22.8<br />

5.1<br />

21.7<br />

21.7<br />

20.0<br />

21.2<br />

22.2<br />

21,9<br />

22.5<br />

5.6<br />

22.5<br />

La<br />

381.0<br />

447.0<br />

443.0<br />

542.0<br />

451.0<br />

569.0<br />

780.0<br />

140.0<br />

514.0<br />

520.0<br />

512.0<br />

410.0<br />

477.0<br />

443.0<br />

406.0<br />

445.0<br />

461.0<br />

436.0<br />

739.0<br />

488. 0<br />

399.0<br />

351.0<br />

405.0<br />

402.0<br />

389.0<br />

466.0<br />

373.0<br />

313.0<br />

319.0<br />

473.0<br />

596.0<br />

29.0<br />

443.0<br />

442.0<br />

487.0<br />

448.0<br />

409.0<br />

329.0<br />

395.0<br />

327.0<br />

353.0<br />

365.0<br />

495.0<br />

629.0<br />

763.0<br />

691.0<br />

33.0<br />

332.0<br />

317.0<br />

324.0<br />

344.0<br />

392.0<br />

380.0<br />

293.0<br />

28.0<br />

404.0<br />

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3.0<br />

6.0<br />

10.0<br />

1.0<br />

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7.0<br />

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2.0<br />

2.0<br />

-2.0<br />

1.0<br />

2.0<br />

-1.0<br />

-1.0<br />

2.0<br />

4.0<br />

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3.0<br />

4.0<br />

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15.0<br />

3.0<br />

7.0<br />

7.0<br />

7.0<br />

-3.0<br />

8.0<br />

2.0<br />

6.0<br />

1.0<br />

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1.0<br />

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-1.0<br />

-1.0<br />

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5.0<br />

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13.0<br />

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8.0<br />

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5.0<br />

2.0<br />

1.0<br />

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2.0<br />

8.0<br />

7.0<br />

4.0<br />

9.0<br />

2.0<br />

5.0<br />

Ni<br />

170.0<br />

130.0<br />

150.0<br />

120.0<br />

110.0<br />

88.0<br />

120.0<br />

250.0<br />

33.0<br />

-23.0<br />

190.0<br />

130.0<br />

31.0<br />

85.0<br />

92.0<br />

86.0<br />

64.0<br />

64.0<br />

120.0<br />

55.0<br />

54.0<br />

130.0<br />

46.0<br />

47.0<br />

140.0<br />

49.0<br />

97.0<br />

91.0<br />

130.0<br />

-27.0<br />

-29.0<br />

52.0<br />

62.0<br />

49.0<br />

58.0<br />

110.0<br />

90.0<br />

97.0<br />

140.0<br />

140.0 '<br />

99.0<br />

96,0<br />

93.0<br />

60.0<br />

-34.0<br />

-33.0<br />

B3.0<br />

73.0<br />

61.0<br />

-24.0<br />

37.0<br />

59.0<br />

49.0<br />

160.0<br />

90.0<br />

BO.O<br />

Rb<br />

-12.0<br />

-13.0<br />

19.0<br />

25.0<br />

-12.0<br />

-12.0<br />

18.0<br />

95.0<br />

16.0<br />

-13.0<br />

22.0<br />

12.0<br />

12.0<br />

16.0<br />

-5.0<br />

12.0<br />

14.0<br />

-11.0<br />

26.0<br />

20.0<br />

-15.0<br />

-15.0<br />

-15.0<br />

-16.0<br />

-16.0<br />

-18.0<br />

16.0<br />

-13.0<br />

-15.0<br />

-15.0<br />

-17.0<br />

98.0<br />

-16.0<br />

-14.0<br />

-16.0<br />

20.0<br />

16.0<br />

-13.0<br />

31.0<br />

-14.0<br />

-16.0<br />

-15.0<br />

-18.0<br />

-19.0<br />

-19.0<br />

-19.0<br />

110.0<br />

14.0<br />

-14.0<br />

-13.0<br />

21.0<br />

22.0<br />

-15.0<br />

15.0<br />

120.0<br />

-14.0<br />

Se<br />

87.7<br />

B6.3<br />

92.5<br />

B9.3<br />

82.8<br />

81.5<br />

73.5<br />

18.0<br />

99.0<br />

102.0<br />

100.0<br />

86.0<br />

92.2<br />

93.4<br />

B9.5<br />

94.7<br />

91.5<br />

87.5<br />

137.0<br />

97.0<br />

82.1<br />

77.4<br />

83.4<br />

76. 5<br />

70.3<br />

63.8<br />

68.6<br />

74.2<br />

78.2<br />

83.2<br />

90.4<br />

15.0<br />

78.2<br />

81. 1<br />

B6.2<br />

7B.8<br />

81.6<br />

74.3<br />

77.6<br />

74.3<br />

63.6<br />

72.2<br />

78.8<br />

B4.9<br />

81.2<br />

81.7<br />

18.0<br />

77.7<br />

83.6<br />

B3.6<br />

90.2<br />

92.3<br />

89.1<br />

81.9<br />

20.4<br />

78.0<br />

>>> H M c


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31<br />

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18<br />

19<br />

20<br />

21.2<br />

21.3<br />

22.8<br />

22.1<br />

19,0<br />

20.8<br />

21.7<br />

20.3<br />

19.0<br />

20.0<br />

22.3<br />

22.2<br />

22.6<br />

21.B<br />

4.9<br />

21.4<br />

23.2<br />

20.9<br />

24.7<br />

23.4<br />

23.0<br />

18.0<br />

22.6<br />

23,2<br />

22.7<br />

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23.2<br />

20.0<br />

21.0<br />

20.4<br />

20.1<br />

20.1<br />

20.7<br />

20.0<br />

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20.8<br />

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22.0<br />

19.0<br />

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22.8<br />

21.9<br />

21.7<br />

23.0<br />

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329.0<br />

369.0<br />

394.0<br />

360.0<br />

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408.0<br />

388.0<br />

352.0<br />

281.0<br />

287.0<br />

343.0<br />

365.0<br />

357.0<br />

383.0<br />

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554.0<br />

459.0<br />

378.0<br />

504.0<br />

507.0<br />

502.0<br />

306.0<br />

430.0<br />

471.0<br />

444.0<br />

368.0<br />

343.0<br />

331.0<br />

326.0<br />

744.0<br />

632.0<br />

543.0<br />

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555.0<br />

350.0<br />

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478.0<br />

460.0<br />

384.0<br />

398.0<br />

435.0<br />

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384.0<br />

385.0<br />

408.0<br />

418.0<br />

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396.0<br />

377.0<br />

373.0<br />

319.0<br />

392.0<br />

328.0<br />

313.0<br />

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17.0<br />

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9.0<br />

350.0<br />

130.0<br />

90.0<br />

110.0<br />

65.0<br />

76.0<br />

110.0<br />

110.0<br />

85.0<br />

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46.0<br />

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90.0<br />

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73.0<br />

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56.0<br />

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79.0<br />

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-26.0<br />

210.0<br />

83.0<br />

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200.0<br />

160.0<br />

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150.0<br />

110.0<br />

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20.0<br />

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-13.0<br />

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-15.0<br />

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-20.0<br />

-17.0<br />

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16.0<br />

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-17.0<br />

64.0<br />

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-16.0<br />

-14.0<br />

16.0<br />

-14.0<br />

-15.0<br />

-14.0<br />

-15.0<br />

-14.0<br />

-14.0<br />

-15.0<br />

-14.0<br />

13.0<br />

19.0<br />

-15.0<br />

-15.0<br />

-13.0<br />

-14.0<br />

21.0<br />

-13.0<br />

69.2<br />

75.9<br />

79.3<br />

77.1<br />

72.4<br />

68.0<br />

68.0<br />

68.6<br />

72.0<br />

71.4<br />

74.6<br />

60.8<br />

84.9<br />

BO.l<br />

14.0<br />

92.5<br />

85.1<br />

79.0<br />

66.2<br />

92.7<br />

83.6<br />

73.7<br />

B9.0<br />

90.9<br />

87.8<br />

85.5<br />

63.8<br />

70.7<br />

80.0<br />

91.9<br />

88.4<br />

93.0<br />

94.0<br />

B5.3<br />

52.6<br />

17.0<br />

93.3<br />

95.1<br />

80.9<br />

79.1<br />

75.1<br />

64.0<br />

80.6<br />

82.4<br />

80.1<br />

78.6<br />

79.7<br />

71.9<br />

77.7<br />

65.8<br />

78.0<br />

79.7<br />

79.9<br />

B3.5<br />

84.6<br />

83.6<br />

-11.0<br />

-12.0<br />

-13.0<br />

-16.0<br />

-12.0<br />

-18.0<br />

-13.0<br />

-15.0<br />

-12.0<br />

-12.0<br />

-12.0<br />

-14.0<br />

-13.0<br />

-5.0<br />

-5.0<br />

-30.0<br />

-14.0<br />

-14.0<br />

-19.0<br />

-13.0<br />

-19.0<br />

-5.0<br />

-13.0<br />

-13.0<br />

-13.0<br />

-14.0<br />

-15.0<br />

-15.0<br />

-18.0<br />

-16.0<br />

-17.0<br />

-14.0<br />

-14.0<br />

-16.0<br />

-12.0<br />

-5.0<br />

-15.0<br />

-15.0<br />

-13.0<br />

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189.0<br />

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76.7<br />

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66.7<br />

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95.8<br />

91.6<br />

93.2<br />

85.7<br />

88.9<br />

86.3<br />

94.3<br />

89.9<br />

104.0<br />

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85.8<br />

84.6<br />

83.0<br />

87.1<br />

>>> H M c


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RNTBUSH OVERBURDEN DRILLING<br />

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2.0<br />

5.0<br />

7.0<br />

-1.0<br />

-4.0<br />

4.0<br />

5.0<br />

5.0<br />

12.0<br />

10.0<br />

-1.0<br />

7.0<br />

2.0<br />

1.0<br />

1.0<br />

-1.0<br />

-3.0<br />

2.0<br />

-3.0<br />

6.0<br />

-1.0<br />

-4.0<br />

5.0<br />

2.0<br />

-4.0<br />

-1.0<br />

3.0<br />

1.0<br />

4.0<br />

-1.0<br />

15.0<br />

-1.0<br />

2.0<br />

4.0<br />

2.0<br />

4.0<br />

53.0<br />

2.0<br />

3.0<br />

-4.0<br />

1.0<br />

-4.0<br />

-4.0<br />

-1.0<br />

1,0<br />

-4.0<br />

-1.0<br />

7.0<br />

Ni<br />

63.0<br />

-29.0<br />

45.0<br />

45.0<br />

100.0<br />

130.0<br />

82.0<br />

40.0<br />

48.0<br />

92.0<br />

66,0<br />

56.0<br />

67.0<br />

150.0<br />

190.0<br />

160.0<br />

280.0<br />

240.0<br />

130.0<br />

92.0<br />

-37.0<br />

36.0<br />

33.0<br />

-31.0<br />

-31.0<br />

100.0<br />

130.0<br />

140.0<br />

98.0<br />

110.0<br />

100.0<br />

58.0<br />

92.0<br />

62.0<br />

100.0<br />

95.0<br />

120.0<br />

91.0<br />

97.0<br />

38.0<br />

130.0<br />

110.0<br />

92.0<br />

100.0<br />

98.0<br />

110.0<br />

78.0<br />

57.0<br />

130.0<br />

51.0<br />

98.0<br />

150.0<br />

220.0<br />

56.0<br />

58.0<br />

39.0<br />

Rb<br />

-18.0<br />

18.0<br />

-17.0<br />

40.0<br />

-16.0<br />

-16.0<br />

-16.0<br />

28.0<br />

-18.0<br />

23.0<br />

31.0<br />

-19.0<br />

-20.0<br />

-23.0<br />

27.0<br />

23.0<br />

-21.0<br />

25.0<br />

32.0<br />

27.0<br />

-20.0<br />

75.0<br />

17.0<br />

-17.0<br />

-17.0<br />

-19.0<br />

-16.0<br />

-17/0<br />

19. X)<br />

-18.0<br />

-20.0<br />

-20;0<br />

23.0<br />

-19.0<br />

-17.0<br />

-17.0<br />

-24.0<br />

31.0<br />

22.0<br />

-18.0<br />

25.0<br />

-16.0<br />

17.0<br />

-19.0<br />

21.0<br />

160.0<br />

72.0<br />

-20.0<br />

27.0<br />

-21.0<br />

-20.0<br />

19.0<br />

-18.0<br />

-20.0<br />

-27.0<br />

-18.0<br />

Se<br />

93.4<br />

93.1<br />

93.4<br />

i.l<br />

62.5<br />

69.6<br />

77.7<br />

86.1<br />

86.4<br />

86.9<br />

90.1<br />

90.2<br />

94.1<br />

91.5<br />

67.4<br />

91.4<br />

64.0<br />

84.0<br />

96.5<br />

96.2<br />

104.0<br />

il.O<br />

20.6<br />

99.5<br />

95.9<br />

91.8<br />

77.7<br />

87.2<br />

20.4<br />

90.2<br />

92.3<br />

93.1<br />

91.9<br />

95.1<br />

91.4<br />

87.0<br />

106.0<br />

23.5<br />

93.9<br />

95.6<br />

85.9<br />

85.6<br />

G9.8<br />

94.2<br />

71.8<br />

21.7<br />

14.0<br />

95.7<br />

25.3<br />

68.8<br />

86.0<br />

25.9<br />

82.1<br />

93.1<br />

92.5<br />

68.6<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

10 of<br />

ftecor Hole Satp<br />

505 47<br />

506 47<br />

507 47<br />

508 48<br />

509 48<br />

510 49<br />

511 49<br />

512 49<br />

513 49<br />

514 49<br />

515 50<br />

516 51<br />

517 51<br />

518 51<br />

519 51<br />

520 52<br />

521 52<br />

522 52<br />

523 53<br />

524 53<br />

525 54<br />

526 54<br />

527 54<br />

528 54<br />

529 55<br />

530 55<br />

531 55<br />

532 55<br />

533 55<br />

534 55<br />

535 55<br />

536 55<br />

537 56<br />

538 56<br />

539 56<br />

540 56<br />

541 56<br />

542 57<br />

543 57<br />

544 57<br />

545 58<br />

546 58<br />

547 58<br />

548 58<br />

549 59<br />

550 59<br />

551 59<br />

552 59<br />

553 59<br />

554 59<br />

555 60<br />

556 60<br />

557 60<br />

558 60<br />

559 60<br />

560 61<br />

3NTBUSH OVERBURDEN DRILLING<br />

IP<br />

5<br />

6<br />

7<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

3<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

fei<br />

22.2<br />

22,4<br />

B. 5<br />

12,0<br />

13.0<br />

21.0<br />

21.2<br />

21.0<br />

20.7<br />

6.0<br />

7.3<br />

22.1<br />

25.6<br />

7.7<br />

10.0<br />

22.4<br />

23.2<br />

7.5<br />

21.9<br />

0.6<br />

20.8<br />

21.7<br />

20.0<br />

1.9<br />

21.5<br />

20.0<br />

20.0<br />

20.0<br />

18.0<br />

20.3<br />

20.0<br />

7.4<br />

22.9<br />

20.0<br />

23.2<br />

2.7<br />

2.6<br />

19.0<br />

21.2<br />

9.0<br />

22.3<br />

21.0<br />

21.8<br />

5.5<br />

20.4<br />

21.5<br />

21.0<br />

23.7<br />

24.2<br />

11.0<br />

20.8<br />

22.6<br />

20.0<br />

20.0<br />

7.8<br />

19.0<br />

La<br />

394.0<br />

330.0<br />

12.0<br />

13.0<br />

13.0<br />

476.0<br />

414.0<br />

38'7.0<br />

296.0<br />

13.0<br />

10.0<br />

541.0<br />

372.0<br />

15.0<br />

16.0<br />

502.0<br />

422.0<br />

14.0<br />

435.0<br />

19.0<br />

395.0<br />

285.0<br />

277.0<br />

26.0<br />

391.0<br />

403.0<br />

323.0<br />

367.0<br />

361.0 '<br />

433.0 '<br />

461.0<br />

9.0 .<br />

473.0<br />

365.0<br />

553.0<br />

22.0<br />

25.0<br />

472.0<br />

563.0<br />

17.0<br />

531.0<br />

570.0<br />

546.0<br />

18.0<br />

510.0<br />

456.0<br />

517.0<br />

593.0<br />

572.0<br />

14.0<br />

477.0<br />

515.0<br />

460.0<br />

441.0<br />

6.0<br />

498.0<br />

Ho<br />

6.0<br />

7.0<br />

-1,0<br />

2.0<br />

-1.0<br />

-1.0<br />

4.0<br />

8.0<br />

4.0<br />

-1.0<br />

1.0<br />

-1.0<br />

3.0<br />

3.0<br />

1,0<br />

2.0<br />

3.0<br />

1.0<br />

-1,0<br />

2.0<br />

3.0<br />

5.0<br />

-1.0<br />

-1.0<br />

2.0<br />

-3.0<br />

1.0<br />

2.0<br />

6.0<br />

2.0<br />

-3.0<br />

-1.0<br />

-1.0<br />

-1.0<br />

-3.0<br />

-1.0<br />

2.0<br />

-3.0<br />

-3.0<br />

-1.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

2.0<br />

-3.0<br />

-1.0<br />

-3.0<br />

-4.0<br />

-3.0<br />

1.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

5.0<br />

1.0<br />

3.0<br />

Ni<br />

97.0<br />

130.0<br />

120.0<br />

34.0<br />

32.0<br />

-28.0<br />

40.0<br />

39.0<br />

70.0<br />

72.0<br />

120.0<br />

-30.0<br />

63.0<br />

32.0<br />

54.0<br />

-29.0<br />

45.0<br />

60.0<br />

45.0<br />

-20.0<br />

-22.0<br />

94.0<br />

66,0<br />

-20.0<br />

-26.0<br />

-23.0<br />

30.0<br />

68. 0<br />

43.0<br />

-24.0<br />

-24.0<br />

130.0<br />

-26.0<br />

-27.0<br />

-26.0<br />

47.0<br />

30.0<br />

-24.0<br />

43.0<br />

50.0<br />

44.0<br />

-30.0<br />

-26.0<br />

85.0<br />

37.0<br />

55.0<br />

54.0<br />

29.0<br />

58.0<br />

2B.O<br />

45.0<br />

34.0<br />

66.0<br />

150.0<br />

110.0<br />

60,0<br />

Rb<br />

-16.0<br />

-15.0<br />

23.0<br />

30.0<br />

28.0<br />

-16.0<br />

-15.0<br />

15.0<br />

16.0<br />

38.0<br />

40.0<br />

21.0<br />

29.0<br />

84.0<br />

75.0<br />

-16.0<br />

-14.0<br />

21.0<br />

-14.0<br />

33.0<br />

-12.0<br />

-11.0<br />

-11.0<br />

60.0<br />

-14.0<br />

-13.0<br />

-12.0<br />

-13.0<br />

-13.0<br />

-13.0<br />

-14.0<br />

17.0<br />

21.0<br />

25.0<br />

-15.0<br />

63.0<br />

4?,0<br />

-13.0<br />

-16.0<br />

28.0<br />

20.0<br />

-17.0<br />

-15.0<br />

49.0<br />

-15.0<br />

-14.0<br />

-14.0<br />

-15.0<br />

-15.0<br />

9.0<br />

-15.0<br />

-16.0<br />

-14.0<br />

-15.0<br />

14.0<br />

-15.0<br />

Se<br />

71.6<br />

69.9<br />

26.7<br />

25.0<br />

24.1<br />

68.7<br />

79.5<br />

77.3<br />

72.9<br />

31.4<br />

24.6<br />

85.2<br />

65.7<br />

16.0<br />

15.0<br />

75.1<br />

74.9<br />

22.2<br />

76.8<br />

5.3<br />

75.7<br />

62.5<br />

67.6<br />

7.6<br />

78.7<br />

•76.6<br />

69.4<br />

68.4<br />

58.6<br />

71.2<br />

78.1<br />

22.4<br />

84.3<br />

72.0<br />

84.2<br />

6.4<br />

6.2<br />

77.7<br />

83.7<br />

29.2<br />

76.6<br />

80.3<br />

82.2<br />

21.1<br />

83.4<br />

76.4<br />

79.9<br />

79.0<br />

81.2<br />

28.5<br />

77.4<br />

84.2<br />

76,0<br />

65.1<br />

29.7<br />

73.5<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

li of<br />

Recor Hole Saip<br />

561 61<br />

562 61<br />

543 61<br />

564 61<br />

565 61<br />

566 61<br />

567 61<br />

568 61<br />

569 61<br />

570 61<br />

571 61<br />

572 61<br />

573 61<br />

574 62<br />

575 62<br />

576 62<br />

577 62<br />

578 62<br />

579 62<br />

580 62<br />

581 62<br />

582 62<br />

583 62<br />

584 62<br />

585 62<br />

586 63<br />

587 63<br />

588 64<br />

589 64<br />

590 64<br />

591 64<br />

592 65<br />

593 65<br />

594 65<br />

595 65<br />

596 65<br />

597 66<br />

598 66<br />

599 67<br />

600 67<br />

601 67<br />

602 67<br />

603 67<br />

604 67<br />

605 67<br />

606 67<br />

607 68<br />

608 69<br />

609 70<br />

610 70<br />

611 7D<br />

612 71<br />

613 72<br />

614 72<br />

615 72<br />

616 72<br />

RNTBUSH OVERBURDEN DRILLINB<br />

ip<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

8<br />

1<br />

1<br />

1<br />

2<br />

3<br />

1<br />

i<br />

2<br />

3<br />

4<br />

FeX<br />

20.1<br />

19.0<br />

23.8<br />

25.4<br />

22.4<br />

23.3<br />

21.7<br />

24.2<br />

22.9<br />

25.7<br />

24.6<br />

21.6<br />

3.2<br />

27.0<br />

24.2<br />

24.0<br />

22.5<br />

26.8<br />

30.7<br />

25.B<br />

24.2<br />

21.7<br />

21.5<br />

21.6<br />

6.3<br />

22.0<br />

6.1<br />

23.1<br />

22.0<br />

24.4<br />

10,0<br />

23.9<br />

22.4<br />

19.0<br />

20.0<br />

6.9<br />

21.9<br />

2.9<br />

26.4<br />

24.4<br />

24.0<br />

9.2<br />

28.6<br />

28.6<br />

24.6<br />

11,0<br />

7.0<br />

6.9<br />

25.8<br />

23.9<br />

6.1<br />

2.5<br />

25.2<br />

23.1<br />

23.7<br />

10.0<br />

La<br />

466.0<br />

404.0<br />

396.0<br />

346.0<br />

498.0<br />

494.0<br />

545.0<br />

594.0<br />

4B3.0<br />

554.0<br />

429.0<br />

257.0<br />

16.0<br />

651.0<br />

518.0<br />

453.0<br />

481.0<br />

514.0<br />

311.0<br />

525.0<br />

354.0<br />

402.0<br />

373.0<br />

400.0<br />

17.0<br />

430.0<br />

18.0<br />

483.0<br />

438.0<br />

579.0<br />

15.0<br />

472.0<br />

377.0<br />

295.0<br />

225.0<br />

17.0<br />

628.0<br />

37.0<br />

639.0<br />

759.0<br />

657.0<br />

6.0<br />

740.0<br />

593.0<br />

590.0<br />

11.0<br />

31.0<br />

28.0<br />

237.0<br />

37.0<br />

11.0<br />

36.0<br />

130.0<br />

634.0<br />

824.0<br />

5.0<br />

ho<br />

4.0<br />

3.0<br />

1.0<br />

-1.0<br />

-1.0<br />

3.0<br />

4,0<br />

-1.0<br />

1.0<br />

-1.0<br />

13.0<br />

6.0<br />

2.0<br />

-1.0<br />

-1.0<br />

-1.0<br />

-1.0<br />

-1.0<br />

4.0<br />

2.0<br />

2.0<br />

-1.0<br />

3.0<br />

1.0<br />

1.0<br />

-1.0<br />

-1.0<br />

3.0<br />

-1.0<br />

-2.0<br />

2.0<br />

-1,0<br />

2.0<br />

1.0<br />

2.0<br />

1.0<br />

-1.0<br />

1.0<br />

1.0<br />

3.0<br />

-1.0<br />

-1.0<br />

3.0<br />

-1.0<br />

-1.0<br />

2.0<br />

2.0<br />

3.0<br />

3.0<br />

4.0<br />

2.0<br />

1.0<br />

4.0<br />

-2.0<br />

6.0<br />

-1.0<br />

Ni<br />

52.0<br />

120.0<br />

76.0<br />

98.0<br />

82.0<br />

110.0<br />

65.0<br />

61.0<br />

51.0<br />

23.0<br />

110.0<br />

88.0<br />

-20.0<br />

66.0<br />

44.0<br />

90.0<br />

90.0<br />

100.0<br />

60.0<br />

71.0<br />

160.0<br />

96.0<br />

85.0<br />

73.0<br />

46.0<br />

120.0<br />

-20.0<br />

47.0<br />

100.0<br />

46.0<br />

-20.0<br />

49.0<br />

60.0<br />

54.0<br />

67.0<br />

71.0<br />

38.0<br />

49.0<br />

390.0<br />

53.0<br />

62.0<br />

73.0<br />

85.0<br />

120.0<br />

87.0<br />

42.0<br />

-20.0<br />

-20,0<br />

71,0<br />

73.0<br />

71.0<br />

-20.0<br />

56.0<br />

29.0<br />

42.0<br />

230.0<br />

Rb<br />

-15.0<br />

-5,0<br />

13.0<br />

14.0<br />

-5.0<br />

-5.0<br />

-10.0<br />

-11.0<br />

-5.0<br />

10.0<br />

-5.0<br />

9.0<br />

32.0<br />

-11.0<br />

14.0<br />

-5.0<br />

9.0<br />

13.0<br />

11.0<br />

10.0<br />

10.0<br />

-5.0<br />

-5.0<br />

10.0<br />

54.0<br />

-5.0<br />

30.0<br />

16.0<br />

14.0<br />

12.0<br />

43.0<br />

16.0<br />

13.0<br />

10.0<br />

12.0<br />

38.0<br />

-11.0<br />

51.0<br />

14.0<br />

-13.0<br />

-12.0<br />

18.0<br />

-14.0<br />

-12.0<br />

-11.0<br />

45.0<br />

26.0<br />

38.0<br />

14.0<br />

14.0<br />

42.0<br />

48.0<br />

13.0<br />

-5.0<br />

-16.0<br />

12.0<br />

Se<br />

73.9<br />

74.0<br />

98.4<br />

77.9<br />

89.7<br />

96.3<br />

98.6<br />

105.0<br />

92.2<br />

103.0<br />

80.5<br />

64.8<br />

8.0<br />

102.0<br />

93.6<br />

91.8<br />

90.8<br />

113.0<br />

68.3<br />

98.4<br />

89.4<br />

84.4<br />

86.5<br />

93.3<br />

25.6<br />

87.9<br />

19.0<br />

114.0<br />

86.7<br />

105.0<br />

34.6<br />

95.3<br />

100.0<br />

82.3<br />

B2.1<br />

22.1<br />

102.0<br />

7.4<br />

90.7<br />

108.0<br />

97.0<br />

39.9<br />

106.0<br />

99.0<br />

93.5<br />

24.3<br />

19.0<br />

18.0<br />

65.5<br />

38.7<br />

19.0<br />

4.6<br />

51.5<br />

94.8<br />

100.0<br />

19.0<br />

>>> H M c


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Page 12 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

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Page<br />

13 of<br />

Recor Hole Satp<br />

673 66<br />

674 66<br />

675 86<br />

676 66<br />

677 66<br />

678 86<br />

679 67<br />

660 67<br />

661 87<br />

682 67<br />

683 88<br />

684 88<br />

685 88<br />

686 88<br />

687 88<br />

688 88<br />

689 88<br />

690 89<br />

691 89<br />

692 89<br />

693 89<br />

694 69<br />

695 69<br />

696 69<br />

697 89<br />

698 89<br />

699 89<br />

700 89<br />

701 90<br />

702 90<br />

703 90<br />

704 90<br />

705 90<br />

706 90<br />

707 90<br />

708 90<br />

709 90<br />

710 90<br />

711 90<br />

712 90<br />

713 90<br />

714 90<br />

715 90<br />

716 91<br />

717 91<br />

716 91<br />

719 91<br />

720 91<br />

721 91<br />

722 91<br />

723 91<br />

724 92<br />

725 92<br />

726 92<br />

727 92<br />

728 93<br />

RNTBUSH OVERBURDEN DRILLING<br />

tp<br />

1<br />

2<br />

3<br />

l<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

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9<br />

10<br />

11 i 2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7 eit4.<br />

3<br />

4<br />

1<br />

Fei<br />

23.9<br />

23.1<br />

27.4<br />

28.9<br />

23.4<br />

8.7<br />

24.4<br />

28.2<br />

24.2<br />

10.0<br />

23.4<br />

26.3<br />

23.0<br />

26.1<br />

27.0<br />

33.6<br />

1.9<br />

26.4<br />

19.0<br />

20.0<br />

22.6<br />

22.2<br />

23.0<br />

21.7<br />

22.3<br />

20.6<br />

23,8<br />

8.9<br />

21.7<br />

21.6<br />

24.9<br />

23.2<br />

22.7<br />

22.6<br />

25.0<br />

22.7<br />

23.1<br />

22.5<br />

19.0<br />

20.1<br />

21.0<br />

23.7<br />

4.3<br />

23.9<br />

24.6<br />

23.6<br />

22.9<br />

22.5<br />

25.2<br />

24.3<br />

12.0<br />

25.5<br />

25.2<br />

25.3<br />

6.1<br />

25.6<br />

La<br />

536.0<br />

574.0<br />

673.0<br />

647.0<br />

506.0<br />

22.0<br />

643.0<br />

461.0<br />

315.0<br />

13.0<br />

712.0<br />

565.0<br />

487.0<br />

696.0<br />

765.0<br />

457.0<br />

32.0<br />

628.0<br />

452.0<br />

428.0<br />

517.0<br />

400.0<br />

433.0<br />

335.0<br />

324.0<br />

332.0<br />

292.0<br />

11.0<br />

504.0<br />

507.0<br />

684.0<br />

503.0<br />

465.0<br />

514.0<br />

326.0<br />

265.0<br />

492.0<br />

346.0<br />

362.0<br />

428.0<br />

473.0<br />

433.0<br />

24.0<br />

555.0<br />

488.0<br />

382.0<br />

371.0<br />

436.0<br />

377.0<br />

410.0<br />

8.0<br />

598.0<br />

555.0<br />

504.0<br />

30.0<br />

433.0<br />

Ho<br />

2.0<br />

-1.0<br />

-1.0<br />

2.0<br />

6.0<br />

1.0<br />

2.0<br />

2.0<br />

2.0<br />

2.0<br />

-1.0<br />

-1.0<br />

5.0<br />

4.0<br />

-1.0<br />

2.0<br />

4.0<br />

3.0<br />

2.0<br />

3.0<br />

3.0<br />

-3.0<br />

-1.0<br />

4.0<br />

4.0<br />

3.0<br />

2.0<br />

1.0<br />

3.0<br />

-3.0<br />

-4.0<br />

2.0<br />

4.0<br />

-1.0<br />

3.0<br />

-3.0<br />

7.0<br />

4.0<br />

5.0<br />

1.0<br />

5.0<br />

2.0<br />

2.0<br />

-3.0<br />

-1.0<br />

-3.0<br />

-3.0<br />

2.0<br />

-2.0<br />

-2.0<br />

-1.0<br />

-3.0<br />

-3.0<br />

-1.0<br />

5.0<br />

2.0<br />

Hi<br />

54.0<br />

58.0<br />

65.0<br />

73.0<br />

110.0<br />

34.0<br />

71.0<br />

120.0<br />

B3.0<br />

-20.0<br />

46.0<br />

300.0<br />

99.0<br />

43.0<br />

92.0<br />

250.0<br />

30.0<br />

-36.0<br />

45.0<br />

-29.0<br />

-35.0<br />

34.0<br />

91.0<br />

76.0<br />

-26.0<br />

42.0<br />

49.0<br />

62.0<br />

41.0<br />

-31.0<br />

36.0<br />

110.0<br />

100.0<br />

39.0<br />

330.0<br />

170.0<br />

61.0<br />

180.0<br />

130.0<br />

51.0<br />

-44.0<br />

69.0<br />

26.0<br />

-32.0<br />

84.0<br />

130.0<br />

110.0<br />

52.0<br />

69.0<br />

69.0<br />

97.0<br />

71.0<br />

83,0<br />

110.0<br />

-20.0<br />

110.0<br />

Rb<br />

19.0<br />

-15.0<br />

18.0<br />

-17.0<br />

-15.0<br />

49.0<br />

-16.0<br />

-15.0<br />

-13.0<br />

31.0<br />

24.0<br />

-16.0<br />

-15.0<br />

-20.0<br />

25.0<br />

-17.0<br />

80.0<br />

-20.0<br />

-13.0<br />

-15.0<br />

-19,0<br />

-16.0<br />

-17.0<br />

-14.0<br />

-13.0<br />

-17.0<br />

-13.0<br />

28.0<br />

-18.0<br />

-17.0<br />

-19.0<br />

-17.0<br />

25.0<br />

-20.0<br />

-17.0<br />

-19.0<br />

-24.0<br />

-21.0<br />

-17.0<br />

-16.0<br />

-25.0<br />

-19.0<br />

69.0<br />

-18.0<br />

-16.0<br />

15.0<br />

-14.0<br />

-16.0<br />

15.0<br />

-13.0<br />

30.0<br />

-16.0<br />

-15.0<br />

-16.0<br />

35.0<br />

-15.0<br />

Se<br />

87.3<br />

88.7<br />

105.0<br />

96.9<br />

88.5<br />

29.3<br />

98.9<br />

89.2<br />

81.5<br />

22.3<br />

92.1<br />

96.0<br />

93.1<br />

104.0<br />

100.0<br />

71.0<br />

6.4<br />

108.0<br />

77.2<br />

92.7<br />

96.6<br />

99.2<br />

101.0<br />

89. 1<br />

90.2<br />

87.4<br />

87.0<br />

31.4<br />

95.8<br />

99.4<br />

101.0<br />

89.9<br />

87.0<br />

95.7<br />

60.8<br />

73.1<br />

103.0<br />

80.7<br />

77.6<br />

68.2<br />

86.3<br />

93.5<br />

7.0<br />

95.6<br />

95.2<br />

87.4<br />

89.9<br />

92.1<br />

93.5<br />

84.8<br />

35.2<br />

96.9<br />

95.9<br />

91.3<br />

11.0<br />

92.1<br />

>>> H M c


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Page<br />

14 of<br />

Recor Hole Satp<br />

729 93<br />

730 93<br />

731 93<br />

732 93<br />

733 93<br />

734 93<br />

735 94<br />

736 94<br />

737 94<br />

738 94<br />

739 94<br />

740 94<br />

741 94<br />

742 94<br />

743 95<br />

744 95<br />

745 95<br />

746 95<br />

747 95<br />

746 95<br />

749 96<br />

750 96<br />

751 96<br />

752 96<br />

753 96<br />

754 96<br />

755 96<br />

756 96<br />

757 96<br />

758 96<br />

759 96<br />

760 96<br />

761 96<br />

762 96<br />

763 96<br />

764 96<br />

765 96<br />

766 97<br />

767 97<br />

768 97<br />

769 97<br />

770 97<br />

771 97<br />

772 97<br />

773 97<br />

774 97<br />

775 97<br />

776 97<br />

777 97<br />

778 97<br />

779 97<br />

780 97<br />

781 97<br />

762 98<br />

783 98<br />

784 98<br />

RNTBUSH OVERBURDEN DRILL<br />

ip<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

17<br />

1<br />

2<br />

3<br />

Fei<br />

24.3<br />

23.3<br />

24.5<br />

25.9<br />

28.0<br />

6.0<br />

23.0<br />

19.0<br />

21.2<br />

22.4<br />

22.0<br />

21.9<br />

21.8<br />

7.2<br />

22.0<br />

20.3<br />

21.3<br />

22.6<br />

21.9<br />

8.0<br />

18.0<br />

21.3<br />

19.0<br />

22.2<br />

22.3<br />

22.0<br />

20.0.<br />

22.1<br />

23.5<br />

22.8<br />

19.0<br />

23.6<br />

21.0<br />

20.7<br />

20.3<br />

21.9<br />

6.9<br />

20.2<br />

22.1<br />

20.2<br />

19.0<br />

21.5<br />

24.9<br />

24.7<br />

25.4<br />

27.0<br />

28.4<br />

25.6<br />

25.5<br />

23.2<br />

23.3<br />

22.7<br />

12.0<br />

24.8<br />

23.2<br />

23.3<br />

La<br />

369.0<br />

391.0<br />

419.0<br />

456.0<br />

436.0<br />

16.0<br />

608.0<br />

505.0<br />

549.0<br />

580.0<br />

532.0<br />

515.0<br />

469.0<br />

11.0<br />

571.0<br />

561.0<br />

557.0<br />

510.0<br />

464.0<br />

11.0<br />

378.0<br />

392.0<br />

327.0<br />

413.0<br />

420.0<br />

371.0<br />

354.0<br />

342.0<br />

331.0<br />

317.0<br />

256.0<br />

453.0<br />

332.0<br />

270.0<br />

266.0<br />

286.0<br />

16.0<br />

493.0<br />

402.0<br />

404.0<br />

358.0<br />

433.0<br />

459.0<br />

442.0<br />

383.0<br />

431.0<br />

446.0<br />

370.0<br />

376.0<br />

33B.O<br />

346.0<br />

314.0<br />

15.0<br />

412.0<br />

358.0<br />

351.0<br />

Mo<br />

-1.0<br />

-2.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

-1.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

-1.0<br />

-3.0<br />

-3.0<br />

-1.0<br />

2.0<br />

-3.0<br />

-3.0<br />

1.0<br />

-3.0<br />

-1.0<br />

-5.0<br />

-6.0<br />

-6.0<br />

-6.0<br />

-6.0<br />

-6.0<br />

-4.0<br />

-4.0<br />

-4.0<br />

-5.0<br />

-3.0<br />

-5.0<br />

-4.0<br />

-4.0<br />

-4.0<br />

-4.0<br />

-1.0<br />

-5.0<br />

-4.0<br />

-4.0<br />

-4.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-4.0<br />

-5.0<br />

-4,0<br />

-4.0<br />

-4.0<br />

-1.0<br />

-5.0<br />

-4.0<br />

-4.0<br />

Ni<br />

120.0<br />

-23.0<br />

-24.0<br />

29.0<br />

30.0<br />

74.0<br />

63.0<br />

-25.0<br />

57.0<br />

32.0<br />

37.0<br />

26.0<br />

31.0<br />

90.0<br />

75.0<br />

56.0<br />

-26.0<br />

52.0<br />

41.0<br />

75.0<br />

49.0<br />

130.0<br />

47.0<br />

45.0<br />

70.0<br />

65.0<br />

65.0<br />

44.0<br />

74.0<br />

180.0<br />

63.0<br />

110.0<br />

78.0<br />

38.0<br />

110.0<br />

86.0<br />

59.0<br />

54.0<br />

-37.0<br />

58.0<br />

68.0<br />

-36.0<br />

-39.0<br />

-36.0<br />

110.0<br />

74.0<br />

41.0<br />

140.0<br />

64.0<br />

62,0<br />

55.0<br />

92.0<br />

58.0<br />

120.0<br />

98.0<br />

110.0<br />

Rb<br />

-13.0<br />

-13.0<br />

-14.0<br />

15.0<br />

-14.0<br />

46.0<br />

-16.0<br />

-14.0<br />

-14.0<br />

-15.0<br />

-14.0<br />

-14.0<br />

-13.0<br />

25.0<br />

-19.0<br />

-14.0<br />

-15.0<br />

-15.0<br />

-15.0<br />

31.0<br />

-16.0<br />

-21.0<br />

-18.0<br />

-18.0<br />

-19.0<br />

-17.0<br />

-17.0<br />

-17.0<br />

-18.0<br />

-30.0<br />

-16.0<br />

-19.0<br />

-17.0<br />

17.0<br />

-18.0<br />

-17.0<br />

32.0<br />

16.0<br />

-20.0<br />

-16.0<br />

-16.0<br />

29.0<br />

-22.0<br />

-19.0<br />

31.0<br />

-19.0<br />

21.0<br />

18.0<br />

-18.0<br />

-16.0<br />

-16.0<br />

-16.0<br />

20.0<br />

-18.0<br />

-17.0<br />

-17.0<br />

ING<br />

Se<br />

86.2<br />

103.0<br />

102.0<br />

106.0<br />

104.0<br />

20.6<br />

89.5<br />

75.5<br />

84.1<br />

90.7<br />

85.7<br />

87.4<br />

93.8<br />

28.7<br />

98.5<br />

89.4<br />

92.7<br />

94.6<br />

90.5<br />

23.2<br />

78.9<br />

88.5<br />

85.6<br />

95.8<br />

92.1<br />

90.6<br />

83.2<br />

90.6<br />

84.8<br />

75.2<br />

69.7<br />

86.9<br />

68.5<br />

88.4<br />

75.7<br />

86.7<br />

21.1<br />

77.2<br />

92.1<br />

91.0<br />

81.9<br />

90.8<br />

97.2<br />

88.6<br />

83.2<br />

91.1<br />

98.8<br />

87.6<br />

91.7<br />

65.3<br />

88.5<br />

84.2<br />

49.2<br />

90.8<br />

91.4<br />

90.8<br />

>>> H M c


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Page 15 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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16 of BURNTBUSH OVERBURDEN DRILLING<br />

Recor Hole Saip fei La Mo Ni Rb Se<br />

841<br />

842<br />

843<br />

644<br />

845<br />

646<br />

847<br />

648<br />

849<br />

850<br />

651<br />

852<br />

653<br />

854<br />

855<br />

856<br />

857<br />

858<br />

859<br />

860<br />

861<br />

862<br />

863<br />

864<br />

865<br />

866<br />

867<br />

868<br />

869<br />

870<br />

871<br />

872<br />

873<br />

874<br />

875<br />

876<br />

877<br />

878<br />

879<br />

880<br />

881<br />

882<br />

883<br />

884<br />

835<br />

886<br />

887<br />

888<br />

689<br />

890<br />

891<br />

892<br />

893<br />

894<br />

895<br />

896<br />

102<br />

102<br />

102<br />

102<br />

102<br />

102<br />

102<br />

102<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

103<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

104<br />

105<br />

105<br />

105<br />

105<br />

105<br />

105<br />

105<br />

105<br />

105<br />

106<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

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12<br />

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17<br />

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2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

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9<br />

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21.8<br />

23.0<br />

24.3<br />

26.2<br />

25.9<br />

25.9<br />

25.3<br />

6.2<br />

23.1<br />

24.2<br />

24.2<br />

25.2<br />

22.1<br />

20.3<br />

16.0<br />

17.0<br />

20.2<br />

24.4<br />

25.6<br />

24.4<br />

25.6<br />

24.2<br />

23.1<br />

24.7<br />

27.4<br />

12.0<br />

22.5<br />

25.1<br />

26.4<br />

26.3<br />

24.4<br />

24.3<br />

24.0<br />

20.0<br />

19.0<br />

23.2<br />

18.0<br />

21.7<br />

23.9<br />

21.8<br />

22.0<br />

23.4<br />

24.1<br />

27.2<br />

21.3<br />

6.0<br />

27.8<br />

23.3<br />

22.4<br />

25.0<br />

25.5<br />

24.1<br />

24.4<br />

24. B<br />

12.0<br />

21.4<br />

408 .0 -l .0 130.0<br />

354 .0 -' .0 130.0<br />

308 .0 -lS.O 190.0<br />

520 .0 -4 .0 180.0<br />

363 .0 -' .0 140.0<br />

346 .0 -' .0 130.0<br />

323 .0 -' .0 170.0<br />

10 .0<br />

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385 .0 1.0 71.0<br />

423 .0 -' .0 96.0<br />

447 .0 -f .0 42.0<br />

483 .0 -' .0 97.0<br />

385 .0 -l .0 77.0<br />

449 .0 -' .0 110.0<br />

273 .0 1.0 -36.0<br />

366 .0 -' .0 110.0<br />

357 .0 1.0 69.0<br />

314 .0 -' .0 77.0<br />

314 .0 -' .0 170.0<br />

300 .0 -; 5.0 140.0<br />

307 .0 5.0 130.0<br />

278 .0 -' 1.0 260.0<br />

268 .0<br />

340 .0<br />

270 .0<br />

9 .0<br />

481 .0<br />

383 .0<br />

399 .0<br />

388 .0<br />

386 .0<br />

367 .0<br />

357 .0<br />

313 .0<br />

293 .0<br />

435 .0<br />

257 .0<br />

322 .0<br />

343 .0<br />

283 .0<br />

271 .0<br />

302 .0<br />

214 .0<br />

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160.0<br />

140.0<br />

230.0<br />

98.0<br />

41.0<br />

35.0<br />

76.0<br />

72.0<br />

76.0<br />

84.0<br />

65.0<br />

66.0<br />

120.0<br />

49.0<br />

45.0<br />

77.0<br />

110.0<br />

130.0<br />

100.0<br />

130.0<br />

270.0<br />

449 .0<br />

395 .0<br />

22 .0<br />

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140.0<br />

160.0<br />

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371 .0<br />

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276 .0 -t .0 140.0<br />

322 .0 -:).0 110. 0<br />

324 .0 -: i.O 140.0<br />

294 .0<br />

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140.0<br />

69.0<br />

54.0<br />

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21.0<br />

20.0<br />

-21.0<br />

23.0<br />

-18.0<br />

-18.0<br />

-5.0<br />

-18.0<br />

-19.0<br />

-20.0<br />

-21.0<br />

-20.0<br />

-20.0<br />

19.0<br />

-21.0<br />

18.0<br />

-17.0<br />

-17.0<br />

-17.0<br />

-16.0<br />

-17.0<br />

-18.0<br />

-17.0<br />

-19.0<br />

24.0<br />

-18.0<br />

19.0<br />

-19.0<br />

-19.0<br />

-19.0<br />

19.0<br />

-18.0<br />

-16.0<br />

-16.0<br />

-18.0<br />

-16.0<br />

-17.0<br />

24.0<br />

-16.0<br />

-16.0<br />

-21.0<br />

-17.0<br />

-21.0<br />

23.0<br />

52.0<br />

-25.0<br />

-18.0<br />

32.0<br />

-18.0<br />

20.0<br />

-19.0<br />

18.0<br />

-18.0<br />

14.0<br />

26.0<br />

91.0<br />

93.6<br />

95.3<br />

102.0<br />

101.0<br />

101.0<br />

97.6<br />

23.3<br />

95.5<br />

97.0<br />

98.5<br />

103.0<br />

89.9<br />

84.4<br />

67.7<br />

68.4<br />

85.9<br />

88.7<br />

92.7<br />

92.7<br />

96.4<br />

81.9<br />

82.6<br />

93.9<br />

85.8<br />

42.2<br />

100.0<br />

100.0<br />

102.0<br />

100.0<br />

93.9<br />

92.2<br />

92.3<br />

80.2<br />

79.5<br />

98.4<br />

80.2<br />

95.2<br />

89.7<br />

68.4<br />

89.9<br />

96.4<br />

84.6<br />

114.0<br />

96.3<br />

18.0<br />

112.0<br />

95.1<br />

92.4<br />

93.2<br />

104.0<br />

95.9<br />

97.2<br />

96.6<br />

38.4<br />

98.4<br />

H M C


l l l l l l<br />

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l l l l l l l<br />

l l l<br />

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Recor Hole Saap sp<br />

897 106<br />

B98 106<br />

899 106<br />

900 106<br />

901 106<br />

902 106<br />

903 106<br />

904 106<br />

905 106<br />

906 106<br />

907 106<br />

908 106<br />

909 106<br />

910 106<br />

911 106<br />

912 106<br />

913 106<br />

914 107<br />

915 107<br />

916<br />

917<br />

107<br />

107<br />

918 107<br />

919 107<br />

920 107<br />

921 107<br />

922 107<br />

923 107<br />

924 107<br />

925 107<br />

926 107<br />

927 107<br />

928 107<br />

929 107<br />

930 107<br />

931 107<br />

932 107<br />

933 107<br />

934 107<br />

935 107<br />

936 107<br />

937 108<br />

938 108<br />

939 103<br />

940 108<br />

941 108<br />

942 108<br />

943 108<br />

944 103<br />

945 103<br />

946 108<br />

947 108<br />

948 108<br />

949 108<br />

950 108<br />

951 109<br />

952 109<br />

RNTBUSH OVERBURDEN DRILL ING<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

23<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

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2<br />

fei<br />

22,6<br />

19.0<br />

22.2<br />

23.0<br />

22.1<br />

20.7<br />

18.0<br />

25.7<br />

25.0<br />

25.6<br />

24.3<br />

24.3<br />

20.0<br />

25.0<br />

27.0<br />

27.9<br />

23.9<br />

25.2<br />

22.7<br />

27.2<br />

20.0<br />

23.0<br />

23.8<br />

23.9<br />

24.4<br />

26.3<br />

26.7<br />

24.3<br />

25.3<br />

24.6<br />

22.9<br />

21.4<br />

24.5<br />

26.4<br />

21.6<br />

22.5<br />

23.6<br />

27.6<br />

25.0<br />

6.1<br />

26.2<br />

24.3<br />

19.0<br />

24.6<br />

22.9<br />

24.0<br />

25.0<br />

26.3<br />

26.3<br />

24.8<br />

25.2<br />

27.1<br />

23.7<br />

4.9<br />

25.8<br />

27.7<br />

La<br />

Ho<br />

Ni<br />

464 .0 -5.0 52.0<br />

357 .0 -5.0 35.0<br />

452 .0 -5.0 73.0<br />

424 .0 -5.0 80.0<br />

580 .0<br />

451 .0<br />

381 .0<br />

316 .0<br />

349 .0<br />

313 .0<br />

296 .0<br />

333 .0<br />

-7.0<br />

-6.0<br />

-6.0<br />

-5,0<br />

-5.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

84.0<br />

65.0<br />

56.0<br />

200.0<br />

130.0<br />

180.0<br />

130.0<br />

110.0<br />

190 .0 -3.0 100.0<br />

363 .0 -5.0 140.0<br />

355 .0<br />

393 .0<br />

340 .0<br />

344 .0<br />

517 .0<br />

594 .0<br />

423 .0<br />

485 .0<br />

524 .0<br />

521 .0<br />

463 .0<br />

-5.0<br />

-6.0<br />

-5.0<br />

-5.0<br />

-6.0<br />

-6.0<br />

-5.0<br />

-6.0<br />

-5.0<br />

-5.0<br />

.0<br />

170.0<br />

180.0<br />

86.0<br />

98.0<br />

49.0<br />

-42.0<br />

36.0<br />

69.0<br />

64.0<br />

-43.0<br />

85.0<br />

390 .0<br />

.0 120.0<br />

34 .0 : 2.0 100.0<br />

501 .0<br />

.0 93.0<br />

486 .0<br />

.0 100.0<br />

449 .0<br />

.0 70.0<br />

473 .0 ' - .0 85.0<br />

499 .0 . - .0 71.0<br />

433 .0<br />

397 .0<br />

455 .0<br />

437 .0<br />

369 .0<br />

-<br />

.0<br />

.0<br />

.0<br />

.0<br />

.0<br />

79.0<br />

61.0<br />

-38.0<br />

110.0<br />

95.0<br />

379 .0<br />

.0 81.0<br />

307 .0<br />

.0 95.0<br />

401 .0<br />

.0 150.0<br />

428 .0<br />

516 .0<br />

302 .0<br />

331 .0<br />

375 .0<br />

362 .0<br />

376 .0<br />

420 .0<br />

554 .0<br />

438 .0<br />

524 .0<br />

476 .0<br />

362 .0<br />

25 .0<br />

419 .0<br />

446 .0<br />

-18.0<br />

-110.0<br />

-3.0<br />

-3.0<br />

-3.0<br />

-4.0<br />

-4,0<br />

-5.0<br />

-5.0<br />

-4.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

1.0<br />

-5.0<br />

-5.0<br />

160.0<br />

220.0<br />

49.0<br />

130.0<br />

57.0<br />

110.0<br />

61.0<br />

110.0<br />

-46.0<br />

-42.0<br />

-45,0<br />

110.0<br />

120.0<br />

35.0<br />

61.0<br />

110.0<br />

Rb<br />

-20.0<br />

-17.0<br />

-19.0<br />

27.0<br />

-25.0<br />

-20.0<br />

-21.0<br />

-19.0<br />

-19.0<br />

-20.0<br />

-18.0<br />

-19.0<br />

-14.0<br />

-19.0<br />

21.0<br />

35.0<br />

-19.0<br />

-18.0<br />

-20.0<br />

-22.0<br />

-18.0<br />

-21.0<br />

-22.0<br />

31.0<br />

-21.0<br />

-22.0<br />

-22.0<br />

-21.0<br />

22.0<br />

-23.0<br />

-20.0<br />

-18.0<br />

-20.0<br />

27.0<br />

-21.0<br />

-19.0<br />

-16.0<br />

-20.0<br />

22.0<br />

110.0<br />

-25.0<br />

-120.0<br />

18.0<br />

19.0<br />

-18.0<br />

-18.0<br />

-18.0<br />

-23.0<br />

-25.0<br />

-22.0<br />

-25.0<br />

-25.0<br />

-24.0<br />

65.0<br />

27.0<br />

-25.0<br />

Se<br />

98.9<br />

81.7<br />

94.3<br />

99.0<br />

93,5<br />

89.2<br />

76.9<br />

91.8<br />

97.7<br />

88.5<br />

90.2<br />

96.0<br />

79.2<br />

95.2<br />

99.3<br />

100.0<br />

95.1<br />

74.6<br />

102.0<br />

110.0<br />

78.9<br />

92.3<br />

89.2<br />

94.4<br />

97.1<br />

101.0<br />

97.9<br />

96.7<br />

102.0<br />

101.0<br />

96.3<br />

101.0<br />

104.0<br />

105.0<br />

86.3<br />

94.1<br />

105.0<br />

105.0<br />

100.0<br />

20.9<br />

79.9<br />

93.5<br />

77.7<br />

94.5<br />

98.9<br />

102.0<br />

101.0<br />

103,0<br />

116.0<br />

110.0<br />

107.0<br />

108.0<br />

94.1<br />

16.0<br />

101.0<br />

100.0<br />

>>> H M c


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Page<br />

18 of BURNTBUSH OVERBURDEN DRILLING<br />

Recor Hole Satp Fei La Ho Ni Rb Se<br />

H M C


l l 19 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


l<br />

l<br />

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Page<br />

Recor<br />

1065<br />

1066<br />

1067<br />

1068<br />

1069<br />

1070<br />

1071<br />

1072<br />

1073<br />

1074<br />

1075<br />

1076<br />

1077<br />

1078<br />

1079<br />

1080<br />

1081<br />

1082<br />

1083<br />

1084<br />

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1109<br />

1110<br />

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1113<br />

1114<br />

1115<br />

1116<br />

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1118<br />

1119<br />

1120<br />

20 of BURNTBUSH OVERBURDEN DRILL<br />

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118<br />

118<br />

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119<br />

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22.8<br />

6.7<br />

18.0<br />

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22.7<br />

23.8<br />

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335.0<br />

266.0<br />

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289.0<br />

313.0<br />

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325.0<br />

342.0<br />

314.0<br />

398.0<br />

289.0<br />

21.0<br />

477.0<br />

352.0<br />

331.0<br />

361.0<br />

338.0<br />

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313.0<br />

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358.0<br />

354.0<br />

403.0<br />

371.0<br />

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610.0<br />

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475.0<br />

490.0<br />

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393,0<br />

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74.0<br />

78.7<br />

83.6<br />

84.2<br />

86.8<br />

81.8<br />

83.7<br />

92.2<br />

85.4<br />

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81.7<br />

92.9<br />

83.2<br />

80.6<br />

90.0<br />

95.4<br />

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84.1<br />

93.0<br />

88.4<br />

87.5<br />

71.7<br />

78.7<br />

75.9<br />

76.1<br />

89.1<br />

84.5<br />

85.4<br />

84.4<br />

78.3<br />

82.5<br />

104.0<br />

106.0<br />

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94.9<br />

99.3<br />

107.0<br />

110.0<br />

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90.8<br />

96.6<br />

87.1<br />

70.8<br />

14.0<br />

83.7<br />

94.0<br />

90.3<br />

>>> HMD


l l Page 21 of BURNTBUSH OVERBURDEN DRILLING H M C


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1185 131<br />

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1193 132<br />

1194 132<br />

1195 132<br />

1196 133<br />

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509.0<br />

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30.5<br />

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94.0<br />

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94.7<br />

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93.3<br />

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>>> H M C


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97.0<br />

-5.0<br />

-5.0<br />

13.0<br />

13.0<br />

-5.0<br />

-5.0<br />

15.0<br />

110.0<br />

9.0<br />

-11.0<br />

-12.0<br />

19.0<br />

100.0<br />

-5.0<br />

-5.0<br />

-5.0<br />

11.0<br />

10.0<br />

-5.0<br />

110.0<br />

12.0<br />

11.0<br />

80. 0<br />

15.0<br />

-5.0<br />

-5.0<br />

12.0<br />

-5.0<br />

-5.0<br />

8.0<br />

97.0<br />

10.0<br />

-5.0<br />

64.0<br />

9.0<br />

Se<br />

68.0<br />

78.6<br />

85.3<br />

B2.0<br />

77.9<br />

74.9<br />

80.0<br />

82. 1<br />

76.2<br />

13.0<br />

79.2<br />

77.0<br />

74.8<br />

73.2<br />

75.2<br />

74.7<br />

76.7<br />

82.3<br />

80.1<br />

90.1<br />

14.0<br />

73.8<br />

Bt.9<br />

79.2<br />

76.4<br />

72.0<br />

62.0<br />

74.0<br />

15.0<br />

75.0<br />

79.4<br />

79.1<br />

77.0<br />

16.0<br />

79.2<br />

76.0<br />

74.9<br />

67.5<br />

70.9<br />

B0.2<br />

16.0<br />

62.1<br />

58.4<br />

19.0<br />

74.5<br />

80.7<br />

76.6<br />

68.6<br />

71.3<br />

57.9<br />

62.3<br />

14.0<br />

78.4<br />

74.0<br />

16.0<br />

72.9<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

l of<br />

Recor Hole Sasp<br />

l<br />

1 l<br />

2 l<br />

3<br />

4<br />

5<br />

6<br />

7<br />

9<br />

10<br />

11 2<br />

12 2<br />

13 2<br />

14 2<br />

15 2<br />

16 2<br />

17 2 2 2<br />

2<br />

18<br />

19<br />

20<br />

21 2<br />

22 3<br />

23 3<br />

24 3<br />

25 3<br />

26 3<br />

27 3<br />

28 3<br />

29 3<br />

30<br />

31<br />

32<br />

33<br />

34<br />

35 5<br />

36 5<br />

37 5<br />

38 5<br />

39 5<br />

40 5<br />

41<br />

42<br />

43<br />

44<br />

45<br />

46<br />

47<br />

48<br />

49<br />

50 7<br />

7<br />

7<br />

51<br />

52<br />

53 8<br />

54 8<br />

55 8<br />

56 9<br />

RNTBUSH OVERBURDEN DRILLING<br />

sp<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

i<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

e<br />

9<br />

10<br />

a i 2<br />

3<br />

4<br />

5<br />

b<br />

7<br />

e i 2<br />

3<br />

4<br />

5<br />

1<br />

2<br />

3<br />

4<br />

5<br />

t<br />

7<br />

1<br />

2<br />

3<br />

1<br />

2<br />

3<br />

4<br />

5<br />

4<br />

7<br />

8<br />

1<br />

2<br />

3<br />

1<br />

y<br />

20.0<br />

le.o<br />

20.1<br />

le.o<br />

14.0<br />

15.0<br />

18.0<br />

20.0<br />

15.0<br />

1.7<br />

19.0<br />

19.0<br />

19.0<br />

20.3<br />

17.0<br />

19.0<br />

16.0<br />

19.0<br />

19.0<br />

21.0<br />

1.6<br />

24.0<br />

24.6<br />

23.8<br />

22.9<br />

20.2<br />

20.1<br />

20.2<br />

2.0<br />

20.0<br />

24.7<br />

29.1<br />

32.3<br />

1.8<br />

17.0<br />

20.0<br />

20,1<br />

16.0<br />

15.0<br />

19.0<br />

2.1<br />

15.0<br />

11.0<br />

2.0<br />

20.6<br />

24,1<br />

22.1<br />

18.0<br />

21.2<br />

15.0<br />

13.0<br />

2.0<br />

22.1<br />

19.0<br />

2.5<br />

18.0<br />

Yb<br />

24.0<br />

27.0<br />

31.0<br />

29.0<br />

25.0<br />

26.0<br />

28.0<br />

29.0<br />

26.0<br />

-2.0<br />

28.0<br />

27.0<br />

27.0<br />

27.0<br />

23.0<br />

28.0<br />

27.0<br />

32.0<br />

29.0<br />

37.0<br />

-2.0<br />

30.0<br />

32.0<br />

32.0<br />

29.0<br />

27.0<br />

22.0<br />

26.0<br />

-2.0<br />

31.0<br />

39.0<br />

39.0<br />

37.0<br />

-2.0<br />

30.0<br />

29.0<br />

26.0<br />

24.0<br />

25.0<br />

30.0<br />

-2.0<br />

24.0<br />

22.0<br />

-2.0<br />

29.0<br />

31.0<br />

31.0<br />

25.0<br />

27.0<br />

IB.O<br />

22.0<br />

-2.0<br />

28.0<br />

27.0<br />

-2.0<br />

27.0<br />

2n<br />

-100.0<br />

120.0<br />

110.0<br />

170.0<br />

100.0<br />

150.0<br />

140.0<br />

140.0<br />

150.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

110.0<br />

-100.0<br />

110.0<br />

120.0<br />

130.0<br />

200.0<br />

180.0<br />

180.0<br />

130.0<br />

-100.0<br />

-100.0<br />

120.0<br />

-100.0<br />

-100.0<br />

120.0<br />

140.0<br />

170.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

110.0<br />

120.0<br />

110.0<br />

170.0<br />

110.0<br />

340.0<br />

160.0<br />

160.0<br />

150.0<br />

-100.0<br />

-100.0<br />

150.0<br />

140.0<br />

150.0<br />

110.0<br />

110,0<br />

130.0<br />

130.0<br />

150.0<br />

-100.0<br />

130.0<br />

140.0<br />

-100.0<br />

160.0<br />

Ce<br />

460.0<br />

547.0<br />

573.0<br />

548.0<br />

480.0<br />

538.0<br />

568.0<br />

645.0<br />

516.0<br />

37.0<br />

532.0<br />

490.0<br />

516.0<br />

576.0<br />

490.0<br />

532.0<br />

559.0<br />

684.0<br />

641.0<br />

771.0<br />

50.0<br />

623.0<br />

702.0<br />

673.0<br />

590.0<br />

557.0<br />

510.0<br />

529.0<br />

51.0<br />

723.0<br />

1060.0<br />

1280.0<br />

1120.0<br />

58.0<br />

574.0<br />

560.0<br />

560.0<br />

490.0<br />

480.0<br />

566.0<br />

38.0<br />

554.0<br />

460.0<br />

50.0<br />

601.0<br />

671.0<br />

642.0<br />

547.0<br />

580. 0<br />

330.0<br />

440.0<br />

54.0<br />

618.0<br />

557.0<br />

54.0<br />

524.0<br />

Nal<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.2<br />

0.2<br />

0.3<br />

2.6<br />

0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

0.2<br />

0.2<br />

0.2<br />

0.2<br />

2.4<br />

0.3<br />

0.2<br />

0.2<br />

0.3<br />

0.4<br />

0.3<br />

0.4<br />

2.7<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

2.0<br />

0.2<br />

0.2<br />

0.2<br />

0.3<br />

0.4<br />

0.2<br />

2.0<br />

0.3<br />

0.3<br />

2.9<br />

0.3<br />

0.3<br />

0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

3.1<br />

0.2<br />

0.3<br />

2.1<br />

0.4<br />

Sn<br />

-100.0<br />

-100.0<br />

220.0<br />

190.0<br />

160.0<br />

130.0<br />

190.0<br />

130.0<br />

170.0<br />

-100.0<br />

110.0<br />

110.0<br />

140.0<br />

110.0<br />

120.0<br />

150.0<br />

110.0<br />

-100.0<br />

110.0<br />

300.0<br />

-100.0<br />

240.0<br />

210.0<br />

140.0<br />

200.0<br />

200.0<br />

120.0<br />

210.0<br />

-100.0<br />

240.0<br />

210.0<br />

160.0<br />

350.0<br />

-100.0<br />

-100.0<br />

130.0<br />

150.0<br />

160.0<br />

110.0<br />

180.0<br />

-100.0<br />

-100.0<br />

130.0<br />

-100.0<br />

-100.0<br />

160.0<br />

150.0<br />

-100.0<br />

190.0<br />

110.0<br />

-100.0<br />

-100.0<br />

190.0<br />

180.0<br />

-100.0<br />

160.0<br />

>>> H M C


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

2 of BURNTBUSH OVERBURDEN DRILLING >>> HMD


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

3 of<br />

Recor Hole Sacp<br />

113 17<br />

114 17<br />

115 17<br />

114 17<br />

117 17<br />

118 17<br />

119 17<br />

120 17<br />

121 17<br />

122 17<br />

123 17<br />

124 17<br />

125 17<br />

124 17<br />

127 17<br />

128 17<br />

129 17<br />

130 17<br />

131 18<br />

132 18<br />

133 18<br />

134 18<br />

135 18<br />

134 18<br />

137 19<br />

138 19<br />

139 19<br />

140 19<br />

141 19<br />

142 19<br />

143 19<br />

144 20<br />

145 20<br />

146 20<br />

147 20<br />

148 20<br />

149 20<br />

150 20<br />

151 20<br />

152 20<br />

153 20<br />

154 20<br />

155 20<br />

156 20<br />

157 20<br />

158 20<br />

159 20<br />

160 21<br />

161 21<br />

162 21<br />

163 21<br />

164 21<br />

165 21<br />

166 21<br />

167 21<br />

168 21<br />

RNTBUSH OVERBURDEN DRILL<br />

up<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

!i<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

U<br />

22.5<br />

19.0<br />

24.0<br />

21.6<br />

25.3<br />

22.6<br />

22.5<br />

24.1<br />

24.2<br />

21.6<br />

17.0<br />

10.0<br />

17.0<br />

23.9<br />

24.4<br />

28.5<br />

24.4<br />

1.9<br />

21.1<br />

23.3<br />

24.8<br />

27.9<br />

19.0<br />

1.6<br />

23.6<br />

23.6<br />

18.0<br />

21.4<br />

21.4<br />

18.0<br />

1.9<br />

15.0<br />

14.0<br />

16.0<br />

29.4<br />

23.7<br />

23.9<br />

24.7<br />

21,5<br />

25.2<br />

20.0<br />

20.6<br />

23.2<br />

24.4<br />

20.0<br />

18.0<br />

1.6<br />

26.0<br />

23.6<br />

21.2<br />

20.3<br />

20.8<br />

21,5<br />

20.8<br />

14.0<br />

21.6<br />

Yb<br />

28.0<br />

24.0<br />

31.0<br />

28.0<br />

32.0<br />

31.0<br />

34.0<br />

31.0<br />

35.0<br />

33.0<br />

29.0<br />

20.0<br />

32.0<br />

36.0<br />

35.0<br />

40.0<br />

39.0<br />

-2.0<br />

33.0<br />

38.0<br />

34.0<br />

43.0<br />

29.0<br />

-2.0<br />

34.0<br />

33.0<br />

31.0<br />

36.0<br />

34.0<br />

38.0<br />

-2.0<br />

28.0<br />

32.0<br />

32.0<br />

35.0<br />

34.0<br />

32.0<br />

32.0<br />

33.0<br />

36.0<br />

31.0<br />

37.0<br />

35.0<br />

30.0<br />

24.0<br />

28.0<br />

-2.0<br />

28.0<br />

33.0<br />

31.0<br />

31.0<br />

31.0<br />

31.0<br />

31.0<br />

24.0<br />

32.0<br />

Zn<br />

160.0<br />

140.0<br />

140.0<br />

-100.0<br />

150.0<br />

120.0<br />

150.0<br />

-100.0<br />

200.0<br />

-100.0<br />

150.0<br />

180.0<br />

180.0<br />

210.0<br />

180.0<br />

-100.0<br />

200.0<br />

120.0<br />

150.0<br />

240.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

110.0<br />

-100.0<br />

170.0<br />

150.0<br />

-100.0<br />

150.0<br />

-100.0<br />

140.0<br />

100.0<br />

-100.0<br />

100.0<br />

120.0<br />

130.0<br />

-100.0<br />

-100.0<br />

180.0<br />

160.0<br />

-100.0<br />

120.0<br />

170.0<br />

220.0<br />

-100.0<br />

170.0<br />

150.0<br />

130.0<br />

-100.0<br />

-100.0<br />

140.0<br />

170.0<br />

140,0<br />

190.0<br />

-100.0<br />

120.0<br />

Ce<br />

586.0<br />

542.0<br />

631.0<br />

621.0<br />

692.0<br />

629.0<br />

680.0<br />

772.0<br />

754.0<br />

739.0<br />

770.0<br />

440.0<br />

643.0<br />

944.0<br />

906.0<br />

995.0<br />

809.0<br />

41.0<br />

755.0<br />

818.0<br />

837.0<br />

1500.0<br />

932.0<br />

89.0<br />

769.0<br />

775.0<br />

444.0<br />

948.0<br />

831.0<br />

820.0<br />

49.0<br />

686.0<br />

673.0<br />

697.0<br />

791.0<br />

861.0<br />

746.0<br />

748.0<br />

668.0<br />

723.0<br />

607.0<br />

804.0<br />

1070.0<br />

929.0<br />

822.0<br />

859.0<br />

51.0<br />

790.0<br />

815.0<br />

690,0<br />

647.0<br />

681.0<br />

655.0<br />

633.0<br />

535.0<br />

720.0<br />

M<br />

0.3<br />

0.4<br />

0.3<br />

0.4<br />

0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

-0.1<br />

-0.2<br />

0.3<br />

0.4<br />

-0.3<br />

0.4<br />

2.3<br />

-0.2<br />

0.3<br />

0.4<br />

0.3<br />

-0.2<br />

2.8<br />

-0.2<br />

-0.2<br />

0.2<br />

0.3<br />

-0.2<br />

0.2<br />

2.7<br />

0.3<br />

-0.2<br />

0.2<br />

-0.2<br />

-0.2<br />

0.4<br />

0.3<br />

0.5<br />

0.2<br />

0.2<br />

0.4<br />

0.4<br />

-0.2<br />

0.3<br />

0.3<br />

2,5<br />

0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.6<br />

0.3<br />

ING<br />

Sn<br />

300.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

250.0<br />

190.0<br />

210.0<br />

240.0<br />

210.0<br />

230.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-210.0<br />

-100.0<br />

-240.0<br />

210.0<br />

-100.0<br />

-100.0<br />

-220.0<br />

-100.0<br />

290.0<br />

-200.0<br />

-100.0<br />

410.0<br />

200.0<br />

-100.0<br />

230.0<br />

230.0<br />

190.0<br />

-100.0<br />

-100.0<br />

240.0<br />

210.0<br />

240.0<br />

-100.0<br />

-100.0<br />

190.0<br />

240.0<br />

340.0<br />

-100.0<br />

280.0<br />

300.0<br />

340.0<br />

160.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

220.0<br />

190.0<br />

-100.0<br />

220.0<br />

-100.0<br />

-100.0<br />

190.0<br />

-100.0<br />

>>> HMD


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Page 4 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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Reeor Hole Sasp<br />

225 25<br />

226 25<br />

227 25<br />

228 25<br />

229 25<br />

230 25<br />

231 25<br />

232 25<br />

233 26<br />

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278 28<br />

279 28<br />

280 29<br />

RNTBUSH OVERBURDEN DRILLING<br />

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14<br />

15<br />

16<br />

17<br />

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3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

U<br />

24.0<br />

28.2<br />

25.0<br />

23.5<br />

18.0<br />

22.1<br />

21.6<br />

2.8<br />

27.1<br />

26.6<br />

25.9<br />

20.8<br />

24.9<br />

24.9<br />

23.9<br />

27.9<br />

27.9<br />

25.2<br />

52.5<br />

31.7<br />

26.9<br />

20.0<br />

20.6<br />

23.7<br />

19.0<br />

19.0<br />

18.0<br />

20.0<br />

16.0<br />

19.0<br />

23.4<br />

2.0<br />

23.9<br />

26.2<br />

35.0<br />

25.3<br />

26.8<br />

19.0<br />

23.5<br />

18.0<br />

19.0<br />

20.8<br />

26.7<br />

26.8<br />

30.6<br />

28.3<br />

2.2<br />

20.0<br />

17.0<br />

16.0<br />

19.0<br />

20.2<br />

19.0<br />

16.0<br />

2.2<br />

23.7<br />

Yb<br />

31.0<br />

41.0<br />

37.0<br />

35.0<br />

38.0<br />

32.0<br />

31.0<br />

-2.0<br />

41.0<br />

39.0<br />

39.0<br />

33.0<br />

36.0<br />

33.0<br />

30.0<br />

34.0<br />

34.0<br />

33.0<br />

52.0<br />

33.0<br />

29.0<br />

28.0<br />

33.0<br />

31.0<br />

29.0<br />

30.0<br />

28.0<br />

29.0<br />

28.0<br />

34.0<br />

41.0<br />

-2.0<br />

33.0<br />

33.0<br />

34.0<br />

33.0<br />

32.0<br />

26.0<br />

29.0<br />

29.0<br />

27.0<br />

30.0<br />

35.0<br />

41.0<br />

46.0<br />

43.0<br />

2.0<br />

31.0<br />

32.0<br />

34.0<br />

36.0<br />

37.0<br />

34.0<br />

34.0<br />

-2.0<br />

32.0<br />

2n<br />

-100.0<br />

180.0<br />

-100.0<br />

240.0<br />

150.0<br />

-100.0<br />

-100.0<br />

250.0<br />

190.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

140.0<br />

-100.0<br />

-100.0<br />

190.0<br />

260.0<br />

120.0<br />

190.0<br />

160.0<br />

210.0<br />

240.0<br />

160.0<br />

270.0<br />

190.0<br />

190.0<br />

-100.0<br />

190.0<br />

•230.0<br />

•190.0<br />

-100.0<br />

140.0<br />

: 220.0<br />

150,0<br />

190.0<br />

190.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

170.0<br />

-100.0<br />

-100.0<br />

150.0<br />

-100.0<br />

-100.0<br />

200.0<br />

140.0<br />

-100.0<br />

190.0<br />

-100.0<br />

190.0<br />

150.0<br />

180.0<br />

140.0<br />

140.0<br />

170.0<br />

Ce<br />

724.0<br />

858.0<br />

873.0<br />

979.0<br />

778.0<br />

984.0<br />

1350.0<br />

240.0<br />

976.0<br />

980.0<br />

946.0<br />

789.0<br />

883.0<br />

825.0<br />

751.0<br />

833.0<br />

B26.0<br />

eoo.o<br />

1260.0<br />

665.0<br />

816,0<br />

704.0<br />

791.0<br />

791.0<br />

733.0<br />

926.0<br />

710.0<br />

623.0<br />

666.0<br />

937.0<br />

1140.0<br />

49.0<br />

823.0<br />

838.0<br />

925.0<br />

834.0<br />

769.0<br />

636.0<br />

754.0<br />

653.0<br />

674.0<br />

714.0<br />

946.0<br />

1190.0<br />

1370.0<br />

1260.0<br />

61.0<br />

666.0<br />

634.0<br />

648.0<br />

705.0<br />

775.0<br />

736.0<br />

579.0<br />

54.0<br />

797.0<br />

m<br />

0.3<br />

-0.2<br />

0.3<br />

-0.2<br />

-0.2<br />

0.5<br />

-0.3<br />

2.4<br />

0.4<br />

-0.2<br />

0.4<br />

0.4<br />

-0.2<br />

0.3<br />

0.3<br />

0.4<br />

-0.2<br />

-0.2<br />

0.4<br />

0.3<br />

0.2<br />

0.3<br />

0.2<br />

0.2<br />

0.2<br />

0.4<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

2.7<br />

0.3<br />

0.3<br />

0.3<br />

0.1<br />

0.2<br />

0.2<br />

0.3<br />

0.3<br />

-0.1<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.2<br />

3.2<br />

0.4<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

0.3<br />

2.5<br />

0.3<br />

Sn<br />

180.0<br />

180.0<br />

-100.0<br />

-100.0<br />

290.0<br />

170.0<br />

330.0<br />

-100.0<br />

190.0<br />

220.0<br />

210.0<br />

220.0<br />

150.0<br />

150.0<br />

-100.0<br />

330.0<br />

200.0<br />

220.0<br />

560.0<br />

-100.0<br />

-100.0<br />

270.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

290.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-220.0<br />

-100.0<br />

200.0<br />

-100.0<br />

-210.0<br />

-220.0<br />

-230.0<br />

330.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

200.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

180.0<br />

>>> H M c


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Page<br />

6 of<br />

Recor Hole Saip<br />

281 29<br />

262 29<br />

283 29<br />

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285 29<br />

286 29<br />

287 29<br />

288 29<br />

" 289 29<br />

290 29<br />

291 29<br />

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294 29<br />

295 29<br />

296 30<br />

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298 30<br />

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321 31<br />

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324 31<br />

325 31<br />

326 31<br />

327 31<br />

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329 31<br />

330 31<br />

331 31<br />

332 31<br />

333 31<br />

334 31<br />

335 31<br />

336 31<br />

RNTBUSH OVERBURDEN DRILLING >>><br />

up<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

1<br />

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3<br />

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7<br />

8<br />

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10<br />

11<br />

12<br />

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7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

IB<br />

19<br />

20<br />

U<br />

20.0<br />

20.7<br />

22.3<br />

20.8<br />

20.7<br />

28.1<br />

25.2<br />

23.8<br />

23.0<br />

19.0<br />

22.6<br />

23.B<br />

20.0<br />

15.0<br />

1.0<br />

24.5<br />

27.7<br />

22.9<br />

27.7<br />

27.0<br />

24.9<br />

19.0<br />

22.4<br />

25.7<br />

24.4<br />

23.3<br />

22.0<br />

21.5<br />

20.2<br />

32.3<br />

28.7<br />

21.2<br />

23.0<br />

22.1<br />

16.0<br />

1.1<br />

24.3<br />

26.9<br />

27.8<br />

20.7<br />

20.3<br />

25.3<br />

19.0<br />

25.7<br />

22.9<br />

23.1<br />

25,5<br />

26.5<br />

21.8<br />

26.3<br />

20.8<br />

21.6<br />

18.0<br />

20.6<br />

18.0<br />

17.0<br />

Yb<br />

28.0<br />

30.0<br />

32.0<br />

27.0<br />

27.0<br />

29.0<br />

28.0<br />

26.0<br />

25.0<br />

27.0<br />

29.0<br />

33.0<br />

31.0<br />

28.0<br />

-2.0<br />

33.0<br />

32.0<br />

26.0<br />

33.0<br />

37.0<br />

31.0<br />

25.0<br />

32.0<br />

34.0<br />

33.0<br />

34.0<br />

34.0<br />

28.0<br />

30.0<br />

39.0<br />

40.0<br />

- 35.0<br />

38.0<br />

33.0<br />

21.0<br />

-2.0<br />

38.0<br />

39.0<br />

32.0<br />

29.0<br />

27.0<br />

35.0<br />

27.0<br />

31.0<br />

29.0<br />

31.0<br />

30.0<br />

26.0<br />

27.0<br />

32.0<br />

29.0<br />

32.0<br />

27.0<br />

30.0<br />

30.0<br />

29.0<br />

Zn<br />

140,0<br />

160.0<br />

170.0<br />

-100.0<br />

210.0<br />

140.0<br />

140.0<br />

-100.0<br />

150.0<br />

140.0<br />

150.0<br />

190.0<br />

150.0<br />

180.0<br />

230.0<br />

-100.0<br />

370.0<br />

-100.0<br />

-100.0<br />

150.0<br />

140.0<br />

210.0<br />

150.0<br />

160.0<br />

220.0<br />

150.0<br />

150.0<br />

190.0<br />

290.0<br />

140.0<br />

230.0<br />

190.0<br />

-100.0<br />

150.0<br />

-100.0<br />

180.0<br />

160.0<br />

190.0<br />

150.0<br />

120.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

190.0<br />

120.0<br />

-100.0<br />

150.0<br />

170.0<br />

210.0<br />

200.0<br />

140.0<br />

-100.0<br />

190.0<br />

120.0<br />

190.0<br />

Ce<br />

641.0<br />

742.0<br />

766.0<br />

688.0<br />

637.0<br />

777.0<br />

727.0<br />

569.0<br />

490.0<br />

493.0<br />

576.0<br />

603.0<br />

608.0<br />

629.0<br />

35.0<br />

894.0<br />

730.0<br />

634.0<br />

810.0<br />

811.0<br />

829.0<br />

504.0<br />

734.0<br />

778.0<br />

746.0<br />

648.0<br />

612.0<br />

563.0<br />

587.0<br />

1170.0<br />

1120.0<br />

936.0<br />

1010.0<br />

887.0<br />

555.0<br />

48.0<br />

809.0<br />

814.0<br />

752.0<br />

660.0<br />

681.0<br />

754.0<br />

827.0<br />

766.0<br />

654.0<br />

638.0<br />

708,0<br />

689.0<br />

645.0<br />

673.0<br />

646.0<br />

602.0<br />

559.0<br />

663.0<br />

516.0<br />

538.0<br />

M<br />

0.3<br />

0.3<br />

0.3<br />

0.2<br />

0.4<br />

0.3<br />

0.2<br />

0.3<br />

0.3<br />

0.4<br />

0.2<br />

0.2<br />

0.3<br />

0.4<br />

2.7<br />

0.3<br />

0.4<br />

0.5<br />

0.3<br />

0.3<br />

0.4<br />

0.7<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

0.2<br />

0.2<br />

0.2<br />

0.4<br />

0.2<br />

0.2<br />

0.3<br />

0.4<br />

0.2<br />

3.1<br />

0.3<br />

0.3<br />

0.6<br />

0.5<br />

0.3<br />

0.1<br />

0.4<br />

0.4<br />

0.4<br />

0.4<br />

0.2<br />

-0.1<br />

0.3<br />

0.4<br />

0.2<br />

0.4<br />

0.3<br />

0.2<br />

0.4<br />

0.3<br />

Sn<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

220.0<br />

210.0<br />

2BO.O<br />

-100.0<br />

190.0<br />

250.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-200.0<br />

-100.0<br />

160.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

200.0<br />

210.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

190.0<br />

-220.0<br />

-210.0<br />

-230.0<br />

220.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

210.0<br />

170.0<br />

150.0<br />

-100.0<br />

280.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

180.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

150.0<br />

-100.0<br />

160.0<br />

-100.0<br />

Te<br />

29.0<br />

35.0<br />

31.0<br />

49.0<br />

-24.0<br />

34.0<br />

-30.0<br />

-29.0<br />

31.0<br />

-24.0<br />

-26.0<br />

-28.0<br />

37.0<br />

25.0<br />

-10.0<br />

55.0<br />

29.0<br />

38.0<br />

50.0<br />

50.0<br />

51.0<br />

25.0<br />

-30.0<br />

53.0<br />

-29.0<br />

-28.0<br />

43.0<br />

48.0<br />

-36.0<br />

-35.0<br />

49.0<br />

41.0<br />

45.0<br />

50.0<br />

37.0<br />

-10.0<br />

47.0<br />

33.0<br />

54.0<br />

-24.0<br />

58.0<br />

-29.0<br />

-27.0<br />

39.0<br />

-26.0<br />

32.0<br />

39.0<br />

-28.0<br />

35.0<br />

42.0<br />

-29.0<br />

32.0<br />

-24.0<br />

59.0<br />

54.0<br />

32.0<br />

H M C -<br />

Zr<br />

11000.0<br />

11000.0<br />

12000.0<br />

12000.0<br />

11000.0<br />

16000.0<br />

14000.0<br />

15000.0<br />

13000.0<br />

12000.0<br />

16000.0<br />

18000.0<br />

14000.0<br />

7700.0<br />

240.0<br />

11000.0<br />

14000.0<br />

9600.0<br />

15000.0<br />

14000.0<br />

13000.0<br />

9300.0<br />

13000.0<br />

13000.0<br />

, 14000.0<br />

16000.0<br />

14000.0<br />

15000.0<br />

13000.0<br />

18000.0<br />

15000.0<br />

8600.0<br />

12000.0<br />

13000.0<br />

11000.0<br />

-200.0<br />

15000.0<br />

1BOOO.O<br />

19000.0<br />

12000.0<br />

13000.0<br />

17000.0<br />

13000.0<br />

1BOOO.O<br />

14000.0<br />

12000.0<br />

15000.0<br />

16000.0<br />

12000.0<br />

16000.0<br />

13000.0<br />

14000.0<br />

12000.0<br />

12000.0<br />

11000.0<br />

11000.0<br />


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

i<br />

i<br />

i<br />

i<br />

Page<br />

7 of<br />

Recor Hole Baap<br />

337 31<br />

338 31<br />

339 31<br />

340 31<br />

341 32<br />

342 32<br />

343 32<br />

344 32<br />

345 32<br />

346 32<br />

347 32<br />

348 32<br />

349 32<br />

350 32<br />

351 32<br />

352 32<br />

353 32<br />

354 32<br />

355 33<br />

354 33<br />

357 33<br />

358 33<br />

359 33<br />

360 33<br />

361 33<br />

362 33<br />

363 33<br />

364 33<br />

365 33<br />

366 33<br />

367 33<br />

368 33<br />

369 33<br />

370 34<br />

371 34<br />

372 34<br />

373 34<br />

374 34<br />

375 34<br />

376 34<br />

377 34<br />

378 34<br />

379 34<br />

380 34<br />

381 34<br />

3B2 34<br />

383 34<br />

364 34<br />

385 34<br />

386 34<br />

387 35<br />

388 35<br />

389 35<br />

390 35<br />

391 35<br />

392 35<br />

RNTBUSH OVERBURDEN DRILLING<br />

lap<br />

21<br />

22<br />

23<br />

24<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

1<br />

2<br />

3<br />

4 5 6<br />

7<br />

e<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

1<br />

2<br />

7<br />

4<br />

5<br />

6<br />

U<br />

17,0<br />

17.0<br />

14.0<br />

1.2<br />

20.0<br />

25.9<br />

22.5<br />

25.1<br />

27.7<br />

22.1<br />

27.9<br />

23.5<br />

23.9<br />

14.0<br />

20.3<br />

20.0<br />

20.0<br />

1.0<br />

22.6<br />

38,6<br />

31.3<br />

20.0<br />

16.0<br />

13.0<br />

25.0<br />

23. B<br />

21.0<br />

27.2<br />

24.3<br />

25.6<br />

37.2<br />

34.4<br />

2.1<br />

27.0<br />

23.8<br />

24.5<br />

26.8<br />

23.1<br />

27.2<br />

20.1<br />

21.6<br />

28.9<br />

27.2<br />

27.4<br />

19.0<br />

7.7<br />

23.1<br />

30.9<br />

24.0<br />

25.5<br />

27.6<br />

26.5<br />

28.4<br />

27.5<br />

28,5<br />

27.8<br />

Yb<br />

31.0<br />

31.0<br />

27.0<br />

-2.0<br />

32.0<br />

38. 0<br />

31.0<br />

33.0<br />

32.0<br />

34.0<br />

33.0<br />

27.0<br />

30.0<br />

21.0<br />

32.0<br />

29.0<br />

30.0<br />

-2.0<br />

37.0<br />

44.0<br />

39.0<br />

31.0<br />

25.0<br />

25.0<br />

33.0<br />

32.0<br />

38.0<br />

39.0<br />

33.0<br />

35.0<br />

41.0<br />

39.0<br />

-2.0<br />

34.0<br />

34.0<br />

34.0<br />

30.0<br />

30.0<br />

33.0<br />

29.0<br />

31.0<br />

36.0<br />

36.0<br />

34.0<br />

33.0<br />

15.0<br />

30.0<br />

38.0<br />

35.0<br />

33.0<br />

34.0<br />

34.0<br />

33.0<br />

34.0<br />

34.0<br />

30.0<br />

Zn<br />

200.0<br />

120.0<br />

140.0<br />

130.0<br />

120.0<br />

180.0<br />

150.0<br />

-100.0<br />

170.0<br />

160.0<br />

-100.0<br />

190.0<br />

230.0<br />

210.0<br />

170.0<br />

180.0<br />

170.0<br />

140.0<br />

290.0<br />

320.0<br />

-100.0<br />

120.0<br />

140.0<br />

170.0<br />

370.0<br />

170.0<br />

210.0<br />

170.0<br />

180.0<br />

230.0<br />

-100.0<br />

-100.0<br />

150.0<br />

160.0<br />

240.0<br />

120.0<br />

180.0<br />

160.0<br />

200.0<br />

210.0<br />

170.0<br />

190.0<br />

130.0<br />

170.0<br />

-100.0<br />

140.0<br />

-100.0<br />

150.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

200.0<br />

180.0<br />

180.0<br />

190.0<br />

180.0<br />

Ce<br />

581.0<br />

538.0<br />

494.0<br />

48.0<br />

676.0<br />

923.0<br />

761.0<br />

930.0<br />

701.0<br />

615.0<br />

782.0<br />

655.0<br />

707.0<br />

442.0<br />

640.0<br />

610.0<br />

579.0<br />

44.0<br />

1000.0<br />

1090.0<br />

1210.0<br />

671.0<br />

558.0<br />

526.0<br />

689.0<br />

698.0<br />

695.0<br />

900.0<br />

680.0<br />

745.0<br />

1250.0<br />

1090.0<br />

54.0<br />

749.0<br />

709.0<br />

697.0<br />

713.0<br />

654.0<br />

786.0<br />

496.0<br />

802.0<br />

850.0<br />

841.0<br />

798.0<br />

623.0<br />

301.0<br />

1160.0<br />

1240.0<br />

1200.0<br />

1220.0<br />

914.0<br />

937.0<br />

1040,0<br />

955.0<br />

816.0<br />

714.0<br />

NaX<br />

0.2<br />

0.3<br />

0.3<br />

3.6<br />

0.3<br />

0.3<br />

0.4<br />

-0.2<br />

0.2<br />

0.4<br />

0.4<br />

0.3<br />

0.3<br />

1.0<br />

0.3<br />

0.3<br />

0.3<br />

2.7<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.5<br />

0.4<br />

0.4<br />

0.2<br />

0.2<br />

-0.2<br />

-0.2<br />

-0.2<br />

0.6<br />

-0.3<br />

2.6<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

0.4<br />

0.3<br />

0.3<br />

0.5<br />

0.2<br />

0.2<br />

0.3<br />

0.3<br />

0.4<br />

0.3<br />

0.6<br />

0.3<br />

0.3<br />

0.2<br />

-0.2<br />

0.3<br />

0.3<br />

Sn<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

310.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-220.0<br />

-260.0<br />

-220.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

210.0<br />

-100.0<br />

-230.0<br />

230.0<br />

-200.0<br />

-230.0<br />

240.0<br />

-100.0<br />

-100.0<br />

-220.0<br />

190.0<br />

-100.0<br />

200.0<br />

250.0<br />

-100.0<br />

-210.0<br />

-200.0<br />

-100.0<br />

300.0<br />

260.0<br />

220.0<br />

-210.0<br />

220.0<br />

-210.0<br />

-210.0<br />

-210.0<br />

-260.0<br />

-100.0<br />

320.0<br />

-200.0<br />

200.0<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

8 of<br />

Recor Hole Saip<br />

393 35<br />

394 35<br />

395 35<br />

396 35<br />

397 36<br />

398 36.<br />

399 36<br />

400 36<br />

401 36<br />

402 36<br />

403 36<br />

404 36<br />

405 36<br />

406 36<br />

407 36<br />

408 36<br />

409 36<br />

410 36<br />

411 36<br />

412 36<br />

413 37<br />

414 37<br />

415 37<br />

416 37<br />

417 37<br />

418 37<br />

419 37<br />

420 37<br />

421 37<br />

422 37<br />

423 37<br />

424 37<br />

425 37<br />

426 37<br />

427 37<br />

428 37<br />

429 37<br />

430 37<br />

431 37<br />

432 37<br />

433 37<br />

434 37<br />

435 37<br />

436 38<br />

437 38<br />

438 38<br />

439 38<br />

440 38<br />

441 38<br />

442 38<br />

443 38<br />

444 38<br />

445 38<br />

446 38<br />

447 38<br />

44B 38<br />

RNTBUSH OVERBURDEN DRILLING<br />

tp<br />

7<br />

8<br />

9<br />

10<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

B<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

16<br />

17<br />

18<br />

19<br />

20<br />

21<br />

22<br />

23<br />

1<br />

2<br />

3<br />

4<br />

C<br />

i<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

li<br />

26.0<br />

22.3<br />

22.1<br />

1.9<br />

24.5<br />

25.9<br />

21.8<br />

23.8<br />

22.9<br />

25.9<br />

22.8<br />

20.0<br />

21.4<br />

10.0<br />

17.0<br />

26.4<br />

25.8<br />

25.5<br />

24.4<br />

1.8<br />

21.6<br />

21.1<br />

20.0<br />

21.9<br />

24.1<br />

18.0<br />

21.2<br />

22.7<br />

19.0<br />

15.0<br />

21.5<br />

20.4<br />

19.0<br />

24.0<br />

17.0<br />

20.1<br />

55.0<br />

25.4<br />

24.0<br />

22.5<br />

26,3<br />

21.5<br />

20.2<br />

23.1<br />

25.7<br />

25.3<br />

23,6<br />

21.3<br />

21.8<br />

17.0<br />

20.9<br />

21.6<br />

26.4<br />

21.6<br />

22.3<br />

22.8<br />

Yb<br />

32.0<br />

38.0<br />

38.0<br />

-2.0<br />

34.0<br />

30.0<br />

32.0<br />

33.0<br />

31.0<br />

35.0<br />

34.0<br />

30.0<br />

32.0<br />

31.0<br />

32.0<br />

35.0<br />

34.0<br />

33.0<br />

31.0<br />

-2.0<br />

26,0<br />

24.0<br />

23.0<br />

28.0<br />

28.0<br />

25.0<br />

30.0<br />

28.0<br />

31.0<br />

25,0<br />

32.0<br />

33.0<br />

31.0<br />

34.0<br />

29.0<br />

30.0<br />

42.0<br />

39.0<br />

37.0<br />

40.0<br />

36,0<br />

30.0<br />

33.0<br />

29.0<br />

34,0<br />

34.0<br />

30.0<br />

31.0<br />

29,0<br />

22.0<br />

28,0<br />

29.0<br />

31,0<br />

29.0<br />

30.0<br />

28.0<br />

Zn<br />

190.0<br />

150.0<br />

-100.0<br />

100.0<br />

150.0<br />

190.0<br />

150.0<br />

-100.0<br />

140.0<br />

210.0<br />

150.0<br />

-100.0<br />

230.0<br />

230.0<br />

200.0<br />

180.0<br />

260.0<br />

160.0<br />

190.0<br />

-100.0<br />

220.0<br />

180.0<br />

-100.0<br />

-100.0<br />

160.0<br />

180.0<br />

170.0<br />

220.0<br />

170.0<br />

-100.0<br />

220.0<br />

150.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-320.0<br />

-100.0<br />

-100.0<br />

240.0<br />

-100.0<br />

340.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

240.0<br />

180.0<br />

230.0<br />

140.0<br />

170.0<br />

180.0<br />

190.0<br />

140.0<br />

-100.0<br />

180.0<br />

Ce<br />

732.0<br />

824.0<br />

830.0<br />

45.0<br />

843.0<br />

678.0<br />

706.0<br />

800.0<br />

800.0<br />

722.0<br />

662.0<br />

676.0<br />

770.0<br />

493.0<br />

664.0<br />

840.0<br />

772.0<br />

816.0<br />

809,0<br />

60.0<br />

793.0<br />

728.0<br />

796.0<br />

734.0<br />

666.0<br />

566.0<br />

610.0<br />

600.0<br />

605.0<br />

476.0<br />

673.0<br />

727.0<br />

599.0<br />

895.0<br />

628.0<br />

790.0<br />

2990.0<br />

1080.0<br />

1050.0<br />

927.0<br />

1150.0<br />

941.0<br />

933.0<br />

880.0<br />

872.0<br />

841.0<br />

740.0<br />

701.0<br />

609.0<br />

450.0<br />

603.0<br />

627.0<br />

661.0<br />

622.0<br />

607.0<br />

676.0<br />

Hi*<br />

-0.2<br />

0.3<br />

0.2<br />

2.3<br />

0.5<br />

0.5<br />

0.5<br />

0.3<br />

0.4<br />

0.4<br />

0.4<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

0.2<br />

0.5<br />

0.4<br />

0.4<br />

2.4<br />

0.3<br />

-0.2<br />

0.3<br />

-0.1<br />

-0.1<br />

0.4<br />

0.3<br />

0.3<br />

0.2<br />

0.3<br />

-0.1<br />

0.2<br />

0.3<br />

0.3<br />

0.2<br />

-0.2<br />

-0.4<br />

-0.2<br />

-0.2<br />

0.3<br />

-0.2<br />

-0.2<br />

-0.2<br />

0.5<br />

0.3<br />

-0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.<br />

0.<br />

0.<br />

0.<br />

0.<br />

0.3<br />

0.3<br />

Sn<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

190.0<br />

-100.0<br />

-210.0<br />

-100.0<br />

-100.0<br />

180.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

260.0<br />

-100.0<br />

-100.0<br />

170.0<br />

-100.0<br />

510.0<br />

-230.0<br />

-220.0<br />

-100.0<br />

-200.0<br />

-210.0<br />

320.0<br />

-100.0<br />

-210.0<br />

290.0<br />

-100.0<br />

-250.0<br />

190.0<br />

-220.0<br />

-460.0<br />

270.0<br />

360.0<br />

-220.0<br />

-270.0<br />

290.0<br />

320.0<br />

220.0<br />

-220.0<br />

-210.0<br />

-210.0<br />

280.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

220.0<br />

-100.0<br />

350.0<br />

-200.0<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

'Page<br />

9 of<br />

Recor Hole Sa*p<br />

449 38<br />

450 36<br />

451 38<br />

452 38<br />

453 39<br />

454 39<br />

455 39<br />

456 39<br />

457 39<br />

458 39<br />

459 39<br />

460 39<br />

461 39<br />

462 39<br />

463 39<br />

464 39<br />

465 39<br />

466 39<br />

467 39<br />

468 39<br />

469 39<br />

470 39<br />

471 40<br />

472 41<br />

473 41<br />

474 41<br />

475 41<br />

476 41<br />

477 41<br />

478 42<br />

479 42<br />

480 42<br />

481 42<br />

482 42<br />

483 42<br />

484 42<br />

485 42<br />

486 42<br />

487 43<br />

488 43<br />

489 43<br />

490 43<br />

491 43<br />

492 43<br />

493 43<br />

494 43<br />

495 44<br />

496 45<br />

497 45<br />

498 46<br />

499 46<br />

500 46<br />

501 47<br />

502 47<br />

503 47<br />

504 47<br />

RNTBUSH OVERBURDEN DRILLINB<br />

up<br />

14<br />

15<br />

16<br />

17<br />

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30.5<br />

23.1<br />

22.5<br />

1.1<br />

21.6<br />

22.7<br />

20.7<br />

25.9<br />

27.7<br />

27.7<br />

26.1<br />

27.8<br />

24.7<br />

27.3<br />

20.9<br />

20.8<br />

18.0<br />

18.0<br />

24.0<br />

22.0<br />

23.0<br />

0.9<br />

0.2<br />

25.3<br />

20.5<br />

19.0<br />

18.0<br />

20.8<br />

0.3<br />

27.3<br />

26.9<br />

28.0<br />

25.9<br />

25.3<br />

23.8<br />

21.6<br />

28.0<br />

-0.2<br />

24.1<br />

22.0<br />

20.8<br />

16.0<br />

19.0<br />

22.7<br />

15.0<br />

2,2<br />

1.8<br />

44.0<br />

0.4<br />

27.2<br />

27.3<br />

-0.2<br />

25.8<br />

27.2<br />

33.5<br />

24.9<br />

Yb<br />

31.0<br />

31.0<br />

31.0<br />

-2.0<br />

25.0<br />

22.0<br />

25.0<br />

33.0<br />

34.0<br />

34.0<br />

31.0<br />

35.0<br />

34.0<br />

38.0<br />

31.0<br />

33.0<br />

31.0<br />

30.0<br />

37.0<br />

35.0<br />

37.0<br />

-2.0<br />

-2.0<br />

36.0<br />

31.0<br />

29.0<br />

24.0<br />

27.0<br />

2.0<br />

33.0<br />

34.0<br />

35.0<br />

36.0<br />

31.0<br />

32.0<br />

32.0<br />

38,0<br />

2.0<br />

36.0<br />

34.0<br />

31.0<br />

26.0<br />

29.0<br />

36.0<br />

20.0<br />

-2.0<br />

-2.0<br />

36.0<br />

2.0<br />

33.0<br />

30.0<br />

2.0<br />

31.0<br />

31.0<br />

33.0<br />

30.0<br />

Zn<br />

160.0<br />

130.0<br />

-100.0<br />

-100.0<br />

190.0<br />

140.0<br />

180.0<br />

200.0<br />

-100.0<br />

170.0<br />

-100.0<br />

200.0<br />

240.0<br />

-100.0<br />

-100.0<br />

260.0<br />

250.0<br />

210.0<br />

-100.0<br />

280.0<br />

210.0<br />

-100.0<br />

150.0<br />

160.0<br />

180.0<br />

180.0<br />

-100.0<br />

-100.0<br />

160.0<br />

-100.0<br />

170.0<br />

240.0<br />

160.0<br />

220.0<br />

160.0<br />

290.0<br />

220.0<br />

130.0<br />

-100.0<br />

200.0<br />

180.0<br />

160.0<br />

200.0<br />

-100.0<br />

160.0<br />

200.0<br />

150.0<br />

240.0<br />

180.0<br />

230.0<br />

180.0<br />

130.0<br />

180.0<br />

-100.0<br />

240.0<br />

170.0<br />

Ce<br />

812.0<br />

713.0<br />

797.0<br />

52.0<br />

595.0<br />

552.0<br />

606.0<br />

689.0<br />

740.0<br />

766.0<br />

749.0<br />

808.0<br />

685.0<br />

673.0<br />

606.0<br />

695.0<br />

595.0<br />

593.0<br />

725.0<br />

779.0<br />

799.0<br />

43.0<br />

32.0<br />

890.0<br />

641.0<br />

636.0<br />

576.0<br />

616.0<br />

46.0<br />

906.0<br />

972.0<br />

990.0<br />

951.0<br />

858.0<br />

809.0<br />

794.0<br />

893.0<br />

15.0<br />

1010.0<br />

876.0<br />

646.0<br />

577.0<br />

623.0<br />

778.0<br />

584.0<br />

75.0<br />

65.0<br />

1140.0<br />

25.0<br />

1040.0<br />

849.0<br />

25.0<br />

769.0<br />

803.0<br />

986.0<br />

887.0<br />

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0.3<br />

0.4<br />

0.4<br />

4.3<br />

0.5<br />

0.4<br />

0.3<br />

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0.3<br />

0.4<br />

0.4<br />

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0.3<br />

0.4<br />

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0.3<br />

2.3<br />

2.6<br />

-0.2<br />

0.3<br />

0.3<br />

-0.2<br />

0.4<br />

4.3<br />

0.5<br />

0.3<br />

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0.4<br />

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-0.2<br />

0.4<br />

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0.3<br />

0.4<br />

0.4<br />

0.5<br />

0.4<br />

0.3<br />

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2.4<br />

0.4<br />

1.4<br />

0,4<br />

0.5<br />

2.1<br />

0.3<br />

0.6<br />

0.5<br />

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Sn<br />

310.0<br />

220.0<br />

-200.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

220.0<br />

410.0<br />

-220.0<br />

-230.0<br />

-230.0<br />

-230.0<br />

-230.0<br />

-260.0<br />

-230.0<br />

270.0<br />

260.0<br />

-250.0<br />

400.0<br />

280.0<br />

-230.0<br />

-100.0<br />

-100.0<br />

220.0<br />

-100.0<br />

-220.0<br />

-100.0<br />

-200.0<br />

-100.0<br />

-210.0<br />

260.0<br />

-230.0<br />

230.0<br />

-230.0<br />

290.0<br />

-100.0<br />

-280.0<br />

-100.0<br />

340.0<br />

300.0<br />

240.0<br />

-100.0<br />

240.0<br />

320.0<br />

-210.0<br />

-100.0<br />

-100.0<br />

-240.0<br />

-100.0<br />

260.0<br />

420.0<br />

-100.0<br />

-210.0<br />

-240.0<br />

420.0<br />

320.0<br />

>>> H M c


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59<br />

59<br />

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23.0<br />

21.7<br />

-0.2<br />

0.3<br />

0.3<br />

21.2<br />

20.4<br />

19.0<br />

14.0<br />

-0.2<br />

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23.1<br />

19.0<br />

0.5<br />

0.5<br />

27.3<br />

20.0<br />

0.3<br />

20.0<br />

0.6<br />

18.0<br />

13.0<br />

14.0<br />

0.7<br />

20.4<br />

22.7<br />

20.0<br />

20.2<br />

21.9<br />

21.3<br />

21.4<br />

0.2<br />

21.0<br />

17.0<br />

21.7<br />

0.7<br />

0.6<br />

23.8<br />

29.5<br />

-0.2<br />

23,6<br />

26.4<br />

25.8<br />

0,5<br />

25.4<br />

23.4<br />

26.3<br />

27.9<br />

23.8<br />

0.3<br />

25.4<br />

27.4<br />

25.6<br />

25.1<br />

-0.2<br />

26.1<br />

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29.0<br />

27.0<br />

3.0<br />

3.0<br />

3.0<br />

34.0<br />

32.0<br />

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25.0<br />

3.0<br />

2.0<br />

36.0<br />

27.0<br />

2.0<br />

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34.0<br />

30.0<br />

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31.0<br />

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27.0<br />

22.0<br />

25.0<br />

3.0<br />

35.0<br />

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28.0<br />

27.0<br />

23.0<br />

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35.0<br />

29.0<br />

36.0<br />

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33.0<br />

37.0<br />

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33.0<br />

33.0<br />

35.0<br />

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35.0<br />

33.0<br />

36.0<br />

33.0<br />

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32.0<br />

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180.0<br />

250.0<br />

330.0<br />

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220.0<br />

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140.0<br />

150.0<br />

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190.0<br />

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260.0<br />

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140.0<br />

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777.0<br />

654.0<br />

28.0<br />

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26.0<br />

943.0<br />

877.0<br />

799.0<br />

574.0<br />

27.0<br />

24.0<br />

1050.0<br />

714.0<br />

32.0<br />

32.0<br />

975.0<br />

804.0<br />

32.0<br />

840.0<br />

43.0<br />

775.0<br />

555.0<br />

543.0<br />

50.0<br />

769.0<br />

773.0<br />

636.0<br />

741.0<br />

684.0<br />

829.0<br />

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953.0<br />

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0.6<br />

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0.3<br />

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0.2<br />

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0.3<br />

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280.0<br />

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180.0<br />

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260.0<br />

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-100.0<br />

-100.0<br />

220.0<br />

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170.0<br />

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180.0<br />

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210.0<br />

310.0<br />

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-100.0<br />

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260.0<br />

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-100.0<br />

-100.0<br />

200.0<br />

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-100.0<br />

-100.0<br />

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3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

1<br />

2<br />

1<br />

2<br />

T<br />

4<br />

5<br />

6<br />

7<br />

B<br />

1<br />

2<br />

7<br />

4<br />

5<br />

6 t 8<br />

9<br />

10<br />

U<br />

29.1<br />

0.9<br />

21.1<br />

22.8<br />

0.3<br />

0.7<br />

0.9<br />

20.7<br />

19.0<br />

2.0<br />

1.3<br />

22.4<br />

20.5<br />

24.2<br />

21.2<br />

18.0<br />

0.7<br />

27.7<br />

21.2<br />

0.9<br />

16.0<br />

0.7<br />

0.7<br />

25.7<br />

21.4<br />

23.B<br />

24.6<br />

19.0<br />

23.7<br />

22.7<br />

20.5<br />

22,1<br />

21.4<br />

26.7<br />

30.7<br />

1.3<br />

29.4<br />

0.9<br />

28.3<br />

27.2<br />

28.0<br />

20.0<br />

18.0<br />

19.0<br />

19.0<br />

1.6<br />

25.2<br />

23.7<br />

20.6<br />

22.6<br />

34.1<br />

21.7<br />

21.7<br />

19.0<br />

23.0<br />

1.2<br />

Yb<br />

40.0<br />

-2.0<br />

37.0<br />

36.0<br />

3.0<br />

-2.0<br />

-2.0<br />

41.0<br />

37.0<br />

-2.0<br />

-2.0<br />

37.0<br />

33.0<br />

36.0<br />

35.0<br />

34.0<br />

-2.0<br />

37.0<br />

33.0<br />

-2.0<br />

26.0<br />

-2.0<br />

-2.0<br />

35.0<br />

33.0<br />

28.0<br />

35.0<br />

30.0<br />

38.0<br />

38.0<br />

30.0<br />

31.0<br />

36.0<br />

45.0<br />

43.0<br />

-2.0<br />

40.0<br />

-2.0<br />

40.0<br />

40.0<br />

42.0<br />

35.0<br />

32.0<br />

32.0<br />

29.0<br />

-2.0<br />

36.0<br />

30.0<br />

33.0<br />

39.0<br />

45.0<br />

28.0<br />

31.0<br />

32.0<br />

38.0<br />

-2.0<br />

h<br />

140.0<br />

130.0<br />

-100.0<br />

110.0<br />

130.0<br />

130.0<br />

180.0<br />

110.0<br />

150.0<br />

150.0<br />

-100.0<br />

150.0<br />

140.0<br />

160.0<br />

160.0<br />

190.0<br />

130.0<br />

130.0<br />

-100.0<br />

-100.0<br />

110.0<br />

300.0<br />

100.0<br />

150.0<br />

140.0<br />

160.0<br />

150.0<br />

200.0<br />

130.0<br />

130.0<br />

150.0<br />

140.0<br />

120.0<br />

-100.0<br />

110.0<br />

120.0<br />

110.0<br />

110.0<br />

160.0<br />

210.0<br />

220.0<br />

130.0<br />

170.0<br />

150.0<br />

190.0<br />

130.0<br />

130.0<br />

-100.0<br />

110.0<br />

170.0<br />

180.0<br />

120.0<br />

160.0<br />

130.0<br />

160.0<br />

140.0<br />

Ce<br />

1130.0<br />

68.0<br />

965.0<br />

1210.0<br />

25.0<br />

52.0<br />

91.0<br />

860.0<br />

736.0<br />

81.0<br />

60.0<br />

963.0<br />

833.0<br />

877.0<br />

861.0<br />

780.0<br />

62.0<br />

1140.0<br />

837.0<br />

70.0<br />

815.0<br />

42.0<br />

58.0<br />

946.0<br />

850.0<br />

801.0<br />

847.0<br />

693.0<br />

9iB.O<br />

1060.0<br />

818.0<br />

922.0<br />

902.0<br />

1270.0<br />

1430.0<br />

74.0<br />

1150.0<br />

78.0<br />

1160.0<br />

1090.0<br />

1130.0<br />

819.0<br />

669.0<br />

706.0<br />

654.0<br />

58.0<br />

969.0<br />

767.0<br />

692.0<br />

824.0<br />

1410.0<br />

728.0<br />

781.0<br />

790.0<br />

894.0<br />

70.0<br />

NaX<br />

0.5<br />

4.5<br />

-0.3<br />

-0.4<br />

2.2<br />

2.9<br />

5.1<br />

-0.3<br />

0.4<br />

2.6<br />

1.5<br />

-0.3<br />

-0.3<br />

-0.3<br />

-0.3<br />

-0.3<br />

4.6<br />

-0.3<br />

0.3<br />

4.4<br />

-0.3<br />

0.4<br />

3.7<br />

-0.3<br />

-0.3<br />

0.5<br />

-0.3<br />

0.4<br />

0.4<br />

-0.4<br />

0.5<br />

-0.3<br />

-0.4<br />

-0.5<br />

0.8<br />

2.6<br />

-0.4<br />

3.7<br />

0.5<br />

-0.4<br />

-0.5<br />

-0.3<br />

-0.3<br />

-0.3<br />

-0.3<br />

2.0<br />

-0.4<br />

-0.4<br />

0.4<br />

1.1<br />

-0.7<br />

0.2<br />

0.2<br />

0.3<br />

0.3<br />

0.9<br />

Sn<br />

340.0<br />

-100.0<br />

270.0<br />

210.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

310.0<br />

220.0<br />

-100.0<br />

-100.0<br />

260.0<br />

220.0<br />

320.0<br />

160.0<br />

200.0<br />

-100.0<br />

290.0<br />

270.0<br />

-100.0<br />

170.0<br />

-100.0<br />

-100.0<br />

200.0<br />

240.0<br />

230.0<br />

250.0<br />

200.0<br />

280.0<br />

250.0<br />

230.0<br />

230.0<br />

210.0<br />

370.0<br />

310.0<br />

-100.0<br />

300.0<br />

-100.0<br />

310.0<br />

200.0<br />

210.0<br />

270.0<br />

220.0<br />

230.0<br />

210.0<br />

-100.0<br />

280.0<br />

190.0<br />

200.0<br />

210.0<br />

340.0<br />

240.0<br />

360.0<br />

210.0<br />

-100.0<br />

-100.0<br />

>>> H M c


l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

l<br />

Page<br />

13 of<br />

Recor Hole Saip<br />

673 86<br />

674 86<br />

675 86<br />

676 86<br />

677 86<br />

67B 66<br />

679 87<br />

680 87<br />

681 87<br />

682 87<br />

683 63<br />

664 83<br />

685 68<br />

686 B8<br />

687 88<br />

688 8B<br />

689 88<br />

690 89<br />

691 89<br />

692 89<br />

693 89<br />

694 69<br />

695 69<br />

696 69<br />

697 89<br />

698 89<br />

699 89<br />

700 89<br />

701 90<br />

702 90<br />

703 90<br />

704 90<br />

705 90<br />

706 90<br />

707 90<br />

708 90<br />

709 90<br />

710 90<br />

711 90<br />

712 90<br />

713 90<br />

714 90<br />

715 90<br />

716 91<br />

717 91<br />

718 91<br />

719 91<br />

720 91<br />

721 91<br />

722 91<br />

723 91<br />

724 92<br />

725 92<br />

726 92<br />

727 92<br />

726 93<br />

RNTBUSH OVERBURDEN DRILLING<br />

sp<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

1<br />

2<br />

3<br />

4<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

H<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

9<br />

10<br />

11<br />

12<br />

13<br />

14<br />

15<br />

1<br />

2<br />

3<br />

4<br />

5<br />

6<br />

7<br />

8<br />

1<br />

2<br />

3<br />

4<br />

1<br />

U<br />

22.7<br />

27.6<br />

31.0<br />

30.8<br />

20.8<br />

-0.2<br />

25.8<br />

21. B<br />

15.0<br />

0.3<br />

34.5<br />

26.6<br />

23.5<br />

28.5<br />

30.0<br />

21.0<br />

5.0<br />

29.7<br />

24.9<br />

21.8<br />

23.5<br />

16.0<br />

20.3<br />

16.0<br />

15.0<br />

11.0<br />

12.0<br />

0.4<br />

25.3<br />

26.3<br />

29.2<br />

25.4<br />

.21.0<br />

27.2<br />

18.0<br />

18.0<br />

25.2<br />

16.0<br />

20.4<br />

22.6<br />

24.7<br />

21.8<br />

0.7<br />

28.4<br />

24.0<br />

18.0<br />

17.0<br />

22.9<br />

17.0<br />

18.0<br />

-0.2<br />

27.4<br />

25.8<br />

24.3<br />

0.7<br />

22.8<br />

Yb<br />

34.0<br />

36.0<br />

44.0<br />

40.0<br />

35.0<br />

2.0<br />

39.0<br />

34.0<br />

31.0<br />

4.0<br />

39.0<br />

39.0<br />

33.0<br />

43.0<br />

41.0<br />

29.0<br />

3.0<br />

42.0<br />

30.0<br />

33.0<br />

37.0<br />

36.0<br />

35.0<br />

31.0<br />

33.0<br />

28.0<br />

29.0<br />

3.0<br />

35.0<br />

" 40.0<br />

43.0<br />

. 37.0<br />

33.0<br />

38.0<br />

26.0<br />

26.0<br />

39.0<br />

30.0<br />

27.0<br />

31.0<br />

34.0<br />

37.0<br />

-2.0<br />

38.0<br />

37.0<br />

30.0<br />

30.0<br />

37.0<br />

31,0<br />

29.0<br />

3,0<br />

39.0<br />

39.0<br />

35.0<br />

6.0<br />

33.0<br />

Zn<br />

-100.0<br />

-100.0<br />

130.0<br />

-100.0<br />

140.0<br />

160.0<br />

130.0<br />

170.0<br />

210.0<br />

180.0<br />

160.0<br />

150.0<br />

160.0<br />

160.0<br />

200.0<br />

200.0<br />

910.0<br />

170.0<br />

100.0<br />

130.0<br />

140.0<br />

-100.0<br />

260.0<br />

150.0<br />

110.0<br />

270.0<br />

120.0<br />

-100.0<br />

190.0<br />

120.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

220.0<br />

120.0<br />

-100.0<br />

190.0<br />

200.0<br />

210.0<br />

160.0<br />

-100.0<br />

250.0<br />

510.0<br />

140.0<br />

ieo.0<br />

110.0<br />

160. 0<br />

260.0<br />

140.0<br />

220.0<br />

180.0<br />

240.0<br />

170.0<br />

180.0<br />

200.0<br />

210.0<br />

Ce<br />

1010.0<br />

1050.0<br />

1210.0<br />

1180.0<br />

983.0<br />

46.0<br />

1190.0<br />

836.0<br />

590.0<br />

34.0<br />

1400.0<br />

1050.0<br />

909.0<br />

1310.0<br />

1390.0<br />

813.0<br />

62.0<br />

1170.0<br />

785.0<br />

807.0<br />

943.0<br />

744.0<br />

800.0<br />

636.0<br />

625.0<br />

627.0<br />

548.0<br />

26.0<br />

912.0<br />

917.0<br />

1220.0<br />

925.0<br />

847.0<br />

954.0<br />

618.0<br />

490.0<br />

932.0<br />

625.0<br />

615.0<br />

759.0<br />

830.0<br />

768.0<br />

48.0<br />

974.0<br />

841.0<br />

721.0<br />

702.0<br />

805.0<br />

632.0<br />

681.0<br />

19.0<br />

988.0<br />

923.0<br />

872.0<br />

62.0<br />

758.0<br />

m<br />

0.2<br />

0.2<br />

0.5<br />

0.4<br />

0.3<br />

1.9<br />

0.4<br />

0.3<br />

0.3<br />

2.4<br />

0.3<br />

0.2<br />

0.3<br />

0.3<br />

0.3<br />

0.3<br />

2.4<br />

0.3<br />

0.2<br />

0.3<br />

-0.3<br />

0.5<br />

0.3<br />

-0.2<br />

0.3<br />

0.3<br />

0.2<br />

2.2<br />

0.4<br />

0.5<br />

0.6<br />

0.4<br />

0.5<br />

0.4<br />

0.3<br />

0.4<br />

0.5<br />

-0.3<br />

0.3<br />

0.5<br />

-0.2<br />

0.2<br />

1.0<br />

0.4<br />

0.3<br />

0.4<br />

0.3<br />

0.4<br />

0.2<br />

0.3<br />

1.7<br />

0.2<br />

0.3<br />

0.2<br />

3,0<br />

0.4<br />

Sn<br />

160.0<br />

-100.0<br />

370.0<br />

320.0<br />

290.0<br />

-100.0<br />

250.0<br />

250.0<br />

230.0<br />

-100.0<br />

260.0<br />

260.0<br />

-100.0<br />

-230.0<br />

400.0<br />

-100.0<br />

-100.0<br />

-230.0<br />

320.0<br />

-100.0<br />

240.0<br />

350.0<br />

-210.0<br />

-100.0<br />

200.0<br />

-210.0<br />

-100,0<br />

-100.0<br />

230.0<br />

330.0<br />

260.0<br />

-200.0<br />

260.0<br />

310.0<br />

-100.0<br />

210.0<br />

320.0<br />

300.0<br />

-100.0<br />

200.0<br />

-290.0<br />

-220.0<br />

-100.0<br />

250.0<br />

220.0<br />

-100.0<br />

-100.0<br />

210.0<br />

-100.0<br />

170,0<br />

-100.0<br />

220.0<br />

-100.0<br />

250.0<br />

-100.0<br />

-100.0<br />

>>> H M c -c^<br />

Te<br />

33.0<br />

-29.0<br />

-33.0<br />

53.0<br />

-30.0<br />

-10.0<br />

31.0<br />

-28.0<br />

-26.0<br />

-10.0<br />

-34.0<br />

-33.0<br />

-29.0<br />

39.0<br />

-35.0<br />

40.0<br />

-10.0<br />

66.0<br />

-28.0<br />

-32.0<br />

-38.0<br />

-32.0<br />

-36.0<br />

-29.0<br />

-26.0<br />

36.0<br />

-27.0<br />

11.0<br />

46.0<br />

-36.0<br />

-40.0<br />

41.0<br />

-42.0<br />

-39.0<br />

-34.0<br />

39.0<br />

-49.0<br />

-40.0<br />

-34.0<br />

-33.0<br />

-47.0<br />

47.0<br />

-10.0<br />

46.0<br />

37.0<br />

-26.0<br />

27.0<br />

42.0<br />

26.0<br />

35.0<br />

-10.0<br />

63.0<br />

37.0<br />

39.0<br />

-10.0<br />

-28.0<br />

Zr<br />

10000.0<br />

14000.0<br />

18000.0<br />

13000.0<br />

9600.0<br />

270.0<br />

14000.0<br />

12000.0<br />

9500.0<br />

340.0<br />

16000.0<br />

15000.0<br />

15000.0<br />

16000.0<br />

15000.0<br />

10000.0<br />

-200.0<br />

19000.0<br />

17000.0<br />

13000.0<br />

14000.0<br />

9800.0<br />

12000.0<br />

8700.0<br />

4500.0<br />

4300.0<br />

4600.0<br />

-200.0<br />

15000.0<br />

17000.0<br />

14000.0<br />

13000.0<br />

10000.0<br />

15000.0<br />

11000.0<br />

11000.0<br />

15000.0<br />

13000.0<br />

12000.0<br />

13000.0<br />

16000.0<br />

13000.0<br />

260.0<br />

16000.0<br />

15000.0<br />

9200.0<br />

6800.0<br />

16000.0<br />

8800.0<br />

9600.0<br />

-200.0<br />

15000.0<br />

14000.0<br />

14000.0<br />

510.0<br />

14000.0<br />

Br<br />

3.2<br />

-2.0<br />

2.6<br />

-2.0<br />

2.9<br />

-2.0<br />

4.1<br />

-2.0<br />

3.3<br />

-2.0<br />

-2.0<br />

4.6<br />

3.0<br />

7.4<br />

5.1<br />

-2.0<br />

-2.0<br />

-2.0<br />

4.2<br />

2.9<br />

6.2<br />

-2.0<br />

3.3<br />

-2.0<br />

3.5<br />

4.1<br />

-2.0<br />

-2.0<br />

5.7<br />

3.2<br />

3.5<br />

5.4<br />

4.1<br />

-2.0<br />

-2.0<br />

3.1<br />

5.6<br />

3.7<br />

3.0<br />

-2.0<br />

-4.1<br />

6.4<br />

-2.0<br />

2.6<br />

-2.0<br />

2.8<br />

-2.0<br />

2.7<br />

-2.0<br />

3.4<br />

-2.0<br />

-2.0<br />

2.3<br />

-2.0<br />

-2.0<br />

3.4<br />

[87/<br />

Lu<br />

6.0<br />

6.4<br />

7.5<br />

6.6<br />

5.6<br />

0.4<br />

6.5<br />

5.8<br />

5.1<br />

0.7<br />

6.6<br />

6.6<br />

6.0<br />

7.3<br />

7.0<br />

5.1<br />

0.5<br />

7.2<br />

5.3<br />

6.0<br />

6.4<br />

5.9<br />

6.3<br />

5.2<br />

5.4<br />

4.5<br />

4.9<br />

0.4<br />

6.2<br />

6.6<br />

7.4<br />

5.9<br />

5.2<br />

6.1<br />

5.0<br />

4.4<br />

6.7<br />

4.9<br />

4.5<br />

5.4<br />

5.6<br />

6.0<br />

0.3<br />

6.9<br />

6.6<br />

5.1<br />

5.1<br />

6.1<br />

5.4<br />

5.1<br />

0.6<br />

6.6<br />

6.4<br />

6.3<br />

1.0<br />

6.1<br />

12/22]<br />

Si<br />

95.3<br />

100.0<br />

117.0<br />

111.0<br />

97.4<br />

4.3<br />

111.0<br />

81.2<br />

59.3<br />

4.0<br />

141.0<br />

100.0<br />

63.1<br />

117.0<br />

124.0<br />

77.5<br />

3.5<br />

110.0<br />

80.7<br />

77.3<br />

84.5<br />

72.3<br />

75.6<br />

60.8<br />

63.7<br />

58.7<br />

59.3<br />

2.6<br />

83.2<br />

86.9<br />

110.0<br />

67.5<br />

78.9<br />

94.7<br />

59.4<br />

56.4<br />

84.4<br />

56.7<br />

67.8<br />

74.8<br />

63.1<br />

56.0<br />

3.3<br />

70.4<br />

60.4<br />

68.3<br />

65.4<br />

61.0<br />

46.6<br />

50.0<br />

2.9<br />

71.7<br />

68.0<br />

61.7<br />

6.6<br />

55.5


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Page 15 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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Page 16 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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Page 17 of BURNTBUSH OVERBURDEN DRILLING >>> H M C C87/12/223<br />

Recor Hole Saap Yb Zn Ce NaZ Sn Te Ir Br Lu Si<br />

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928<br />

929<br />

930<br />

931<br />

932<br />

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935<br />

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945<br />

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107<br />

107<br />

107<br />

107<br />

107<br />

107<br />

107<br />

108<br />

108<br />

108<br />

108<br />

108<br />

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108<br />

108<br />

108<br />

108<br />

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108<br />

108<br />

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109<br />

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12<br />

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14<br />

1<br />

2<br />

21.6<br />

21.6<br />

22.7<br />

23.0<br />

30.0<br />

24.4<br />

23.6<br />

17.0<br />

17.0<br />

15.0<br />

14.0<br />

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9.3<br />

16.0<br />

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22.4<br />

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23.7<br />

24.4<br />

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22.8<br />

22.4<br />

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19.0<br />

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19.0<br />

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32.0<br />

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36.0<br />

36.0<br />

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30.0<br />

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34.0<br />

30.0<br />

27.0<br />

32.0<br />

19.0<br />

29.0<br />

33.0<br />

34.0<br />

34.0<br />

27.0<br />

39.0<br />

40.0<br />

31.0<br />

34.0<br />

34.0<br />

36.0<br />

34.0<br />

35.0<br />

37.0<br />

36.0<br />

40.0<br />

38.0<br />

38.0<br />

32.0<br />

39.0<br />

36.0<br />

29.0<br />

27.0<br />

27.0<br />

33.0<br />

34.0<br />

2.0<br />

25.0<br />

-37.0<br />

24.0<br />

32,0<br />

34.0<br />

36.0<br />

33.0<br />

35.0<br />

38.0<br />

37.0<br />

39.0<br />

40.0<br />

35.0<br />

-2.0<br />

37.0<br />

38.0<br />

140.0<br />

-100.0<br />

150.0<br />

-100.0<br />

-100.0<br />

190.0<br />

240.0<br />

200.0<br />

210.0<br />

-100.0<br />

-100.0<br />

140.0<br />

170.0<br />

140.0<br />

-100.0<br />

200,0<br />

170.0<br />

-100.0<br />

190.0<br />

160.0<br />

140.0<br />

150.0<br />

-100.0<br />

250.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

270.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

180.0<br />

-100.0<br />

140.0<br />

150.0<br />

180.0<br />

170.0<br />

-100.0<br />

-100.0<br />

250.0<br />

-310.0<br />

190.0<br />

230.0<br />

-100.0<br />

-100.0<br />

230.0<br />

160.0<br />

190.0<br />

160.0<br />

-100.0<br />

230.0<br />

210.0<br />

130.0<br />

180.0<br />

210.0<br />

749.0<br />

656.0<br />

765.0<br />

719.0<br />

1090.0<br />

842.0<br />

701.0<br />

504.0<br />

567.0<br />

555.0<br />

503.0<br />

535.0<br />

350.0<br />

561.0<br />

575.0<br />

614.0<br />

570.0<br />

599.0<br />

828.0<br />

908.0<br />

674.0<br />

793.0<br />

786.0<br />

615.0<br />

709.0<br />

724.0<br />

758.0<br />

741.0<br />

719.0<br />

751.0<br />

686.0<br />

619.0<br />

707.0<br />

631.0<br />

599.0<br />

588.0<br />

420,0<br />

547.0<br />

564.0<br />

54.0<br />

758.0<br />

537.0<br />

534.0<br />

547.0<br />

560.0<br />

586.0<br />

586.0<br />

602.0<br />

756.0<br />

655.0<br />

790.0<br />

724.0<br />

683.0<br />

38.0<br />

628.0<br />

673.0<br />

-0.9<br />

-O.B<br />

-0.9<br />

-O.B<br />

-1.3<br />

-1.0<br />

1.0<br />

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-1.0<br />

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0.5<br />

0.3<br />

0.3<br />

0.5<br />

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0.3<br />

0.3<br />

0.5<br />

0.5<br />

0.4<br />

0.4<br />

0.3<br />

0.5<br />

0.5<br />

0.3<br />

-0.2<br />

2.6<br />

-78.0<br />

-5.0<br />

0.4<br />

0.2<br />

0.3<br />

0.2<br />

0.4<br />

-0.3<br />

0.6<br />

-0.3<br />

-0.3<br />

-0.3<br />

-0.3<br />

3.1<br />

0.4<br />

-0.3<br />

-240.0<br />

220.0<br />

-240.0<br />

-240.0<br />

-310.0<br />

-250.0<br />

-250.0<br />

-220.0<br />

-220.0<br />

-220.0<br />

-210.0<br />

-220.0<br />

-100.0<br />

-230.0<br />

-230.0<br />

-250.0<br />

-220.0<br />

-210.0<br />

320.0<br />

-280.0<br />

-230.0<br />

280.0<br />

-290.0<br />

-290.0<br />

-270.0<br />

-270.0<br />

-270.0<br />

-260.0<br />

-270.0<br />

-270.0<br />

-250.0<br />

-230.0<br />

-250.0<br />

-250.0<br />

-250.0<br />

-230.0<br />

-100.0<br />

-240.0<br />

-240.0<br />

-100.0<br />

-240.0<br />

-900.0<br />

-100.0<br />

-210.0<br />

240.0<br />

240.0<br />

-230.0<br />

-280.0<br />

-300.0<br />

-280.0<br />

-300.0<br />

-300.0<br />

-290.0<br />

-100.0<br />

-290.0<br />

-300.0<br />

-44.0<br />

-40.0<br />

-44.0<br />

-44.0<br />

-74.0<br />

-47.0<br />

-48.0<br />

-42.0<br />

-42.0<br />

-43.0<br />

-40.0<br />

-42.0<br />

-30.0<br />

-43.0<br />

-43.0<br />

-47.0<br />

-42.0<br />

-40.0<br />

-47.0<br />

-53.0<br />

-44.0<br />

-47.0<br />

-48.0<br />

-48.0<br />

-45.0<br />

-53.0<br />

-45.0<br />

-44.0<br />

-44.0<br />

-52.0<br />

-43.0<br />

-38.0<br />

-42.0<br />

-42.0<br />

-42.0<br />

-49.0<br />

-33.0<br />

-46.0<br />

-46.0<br />

-10.0<br />

-68.0<br />

-320.0<br />

-33.0<br />

-36.0<br />

-36.0<br />

-37.0<br />

-39.0<br />

-48.0<br />

-52.0<br />

-47.0<br />

-51.0<br />

-52.0<br />

-49.0<br />

-10.0<br />

-50.0<br />

-52.0<br />

12000.0<br />

12000.0<br />

15000.0<br />

15000.0<br />

16000.0<br />

15000.0<br />

14000.0<br />

11000.0<br />

9900.0<br />

9300.0<br />

9400.0<br />

9300.0<br />

5300.0<br />

10000.0<br />

11000.0<br />

11000.0<br />

10000.0<br />

9600.0<br />

17000.0<br />

17000.0<br />

15000.0<br />

13000.0<br />

17000.0<br />

18000.0<br />

15000.0<br />

14000.0<br />

16000.0<br />

18000.0<br />

18000.0<br />

20000.0<br />

18000.0<br />

14000.0<br />

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5600.0<br />

5400.0<br />

7700.0<br />

6700.0<br />

11000.0<br />

9100.0<br />

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8700.0<br />

6500.0<br />

10000.0<br />

10000.0<br />

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10000.0<br />

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13000.0<br />

11000.0<br />

12000.0<br />

13000.0<br />

11000.0<br />

-200.0<br />

13000.0<br />

16000.0<br />

-4.2<br />

-5.5<br />

-4.1<br />

-4.2<br />

-8.2<br />

-4.7<br />

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-5.6<br />

-4.0<br />

-4.1<br />

-5.5<br />

-5.9<br />

-4.6<br />

-4.0<br />

-4.1<br />

-6.4<br />

-5.9<br />

-5.7<br />

-4.7<br />

8.5<br />

-4.2<br />

-4.7<br />

-2.0<br />

-2.0<br />

-2.0<br />

-2.0<br />

-2.0<br />

. -2.0<br />

-2.0<br />

-2.0<br />

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: -2.0<br />

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3.0<br />

3.7<br />

-2.0<br />

-2.0<br />

-2.0<br />

-2.0<br />

-2.0<br />

-54.0<br />

-750.0<br />

-2.0<br />

-2.0<br />

3.1<br />

-2.0<br />

-2.0<br />

-2.0<br />

-4.2<br />

3.6<br />

-4.2<br />

3.8<br />

-4.5<br />

-2.0<br />

-4.1<br />

-4.3<br />

5.0<br />

4.1<br />

4.9<br />

5.4<br />

5.5<br />

5.5<br />

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.2<br />

.8<br />

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.2<br />

.7<br />

.8<br />

.8<br />

.6<br />

4. B<br />

4.5<br />

4.1<br />

5.1<br />

5.5<br />

4.4<br />

4.7<br />

4.9<br />

5.5<br />

5.2<br />

5.7<br />

5.5<br />

5.6<br />

5.6<br />

5.5<br />

5.3<br />

5.0<br />

5.4<br />

5.0<br />

5.1<br />

5.3<br />

3.6<br />

5.1<br />

4.8<br />

0.4<br />

4.4<br />

-2.8<br />

4.1<br />

4.7<br />

4.7<br />

4.8<br />

4.9<br />

4.9<br />

5.3<br />

5.4<br />

5.2<br />

5.9<br />

5.2<br />

0.2<br />

5.2<br />

5.8<br />

61.8<br />

54.9<br />

59.4<br />

59.4<br />

77.2<br />

40.5<br />

50.4<br />

41.4<br />

43.2<br />

41.1<br />

41.2<br />

43.0<br />

27.3<br />

44.6<br />

45.0<br />

47.6<br />

45.1<br />

51.7<br />

66.4<br />

75.2<br />

66.4<br />

69.1<br />

73.4<br />

67.9<br />

60.9<br />

60.6<br />

58.8<br />

55.6<br />

56.3<br />

57.5<br />

56.0<br />

53.5<br />

57.3<br />

58.9<br />

68.0<br />

65.9<br />

43.2<br />

48.1<br />

47.9<br />

5.6<br />

54.5<br />

53.0<br />

45.0<br />

45.4<br />

47.4<br />

49.4<br />

47.3<br />

48.4<br />

59.7<br />

53.0<br />

61.1<br />

55.2<br />

51.2<br />

4.6<br />

53.0<br />

54.2


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18 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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Page<br />

19 of<br />

Recor Hole Sasp<br />

1009 113<br />

1010 113<br />

1011 113<br />

1012 113<br />

1013 113<br />

1014 113<br />

1015 113<br />

1016 114<br />

1017 114<br />

1018 114<br />

1019 114<br />

1020 114<br />

1021 114<br />

1022 114<br />

1023 114<br />

1024 114<br />

1025 114<br />

1026 114<br />

1027 114<br />

1028 114<br />

1029 114<br />

1030 114<br />

1031 115<br />

1032 115<br />

1033 115<br />

1034 115<br />

1035 115<br />

1036 115<br />

1037 115<br />

1038 115<br />

1039 115<br />

1040 115<br />

1041 115<br />

1042 115<br />

1043 115<br />

1044 115<br />

1045 115<br />

1046 115<br />

1047 115<br />

1048 115<br />

1049 116<br />

1050 116<br />

1051 116<br />

1052 116<br />

1053 116<br />

1054 117<br />

1055 117<br />

1056 117<br />

1057 117<br />

105B 117<br />

1059 117<br />

1060 118<br />

1061 118<br />

1062 118<br />

1063 118<br />

1064 118<br />

RNTBUSH OVERBURDEN DRILLING<br />

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23.5<br />

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19.0<br />

19.0<br />

20.3<br />

1.4<br />

20.0<br />

18.0<br />

18.0<br />

20.7<br />

21.2<br />

28.0<br />

23.1<br />

18.0<br />

21.4<br />

24.8<br />

22.2<br />

23.3<br />

23.7<br />

1.2<br />

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20.0<br />

20.3<br />

16.0<br />

21.6<br />

26.2<br />

24.5<br />

25.0<br />

21.8<br />

19.0<br />

19.0<br />

20.7<br />

16.0<br />

24.0<br />

27.9<br />

20.9<br />

16.0<br />

18.0<br />

1.2<br />

22.1<br />

16,0<br />

20.2<br />

20.0<br />

3.5<br />

18.0<br />

16.0<br />

18.0<br />

20.4<br />

19.0<br />

2.5<br />

20.8<br />

21.0<br />

21.8<br />

22.4<br />

22.6<br />

Yb<br />

27.0<br />

27.0<br />

24.0<br />

33.0<br />

24.0<br />

33.0<br />

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31.0<br />

30.0<br />

29.0<br />

27.0<br />

30.0<br />

32.0<br />

25.0<br />

23.0<br />

28.0<br />

36.0<br />

34.0<br />

40.0<br />

39.0<br />

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32.0<br />

27.0<br />

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28.0<br />

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31.0<br />

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160.0<br />

170.0<br />

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270.0<br />

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-100.0<br />

-100.0<br />

190.0<br />

180.0<br />

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230.0<br />

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140.0<br />

130.0<br />

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180.0<br />

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698.0<br />

661.0<br />

617.0<br />

569.0<br />

591.0<br />

787.0<br />

44.0<br />

686.0<br />

635.0<br />

641.0<br />

650.0<br />

761.0<br />

634.0<br />

543.0<br />

592.0<br />

1030.0<br />

1120.0<br />

1050.0<br />

1150.0<br />

1250.0<br />

36.0<br />

37.0<br />

661.0<br />

611.0<br />

569.0<br />

715.0<br />

678.0<br />

743.0<br />

686.0<br />

634.0<br />

563.0<br />

571.0<br />

584.0<br />

534.0<br />

708.0<br />

1160.0<br />

1020.0<br />

620.0<br />

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21.0<br />

588.0<br />

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681.0<br />

615.0<br />

76.0<br />

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609.0<br />

631.0<br />

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3.7<br />

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0.5<br />

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0.9<br />

0.7<br />

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3.5<br />

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0.7<br />

0.4<br />

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0.8<br />

0.7<br />

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0.5<br />

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0.7<br />

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2.7<br />

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-300.0<br />

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-280.0<br />

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-320.0<br />

390.0<br />

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-290.0<br />

-340.0<br />

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-360.0<br />

-350.0<br />

-100.0<br />

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-280.0<br />

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-270.0<br />

330.0<br />

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-310.0<br />

-380.0<br />

-280.0<br />

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-300.0<br />

-300.0<br />

380.0<br />

-310.0<br />

-400.0<br />

-420.0<br />

-490.0<br />

-320.0<br />

-100.0<br />

310.0<br />

150.0<br />

210.0<br />

-100.0<br />

-100.0<br />

-100.0<br />

-230.0<br />

290.0<br />

200.0<br />

190.0<br />

-100.0<br />

240.0<br />

270.0<br />

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180.0<br />

-100.0<br />

>>> H M C


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1066<br />

1067<br />

1068<br />

1069<br />

1070<br />

1071<br />

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1073<br />

1074<br />

1075<br />

1076<br />

1077<br />

1078<br />

1079<br />

1080<br />

1081<br />

1082<br />

1083<br />

1084<br />

1085<br />

1086<br />

1087<br />

1088<br />

1089<br />

1090<br />

1091<br />

1092<br />

1093<br />

1094<br />

1095<br />

1096<br />

1097<br />

1098<br />

1099<br />

1100<br />

1101<br />

1102<br />

1103<br />

1104<br />

1105<br />

1106<br />

1107<br />

1108<br />

1109<br />

1110<br />

1111<br />

1112<br />

1113<br />

1114<br />

1115<br />

1116<br />

1117<br />

1118<br />

1119<br />

1120<br />

20 of BURNTBUSH OVERBURDEN DRILLING<br />

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118<br />

118<br />

118<br />

119<br />

119<br />

120<br />

120<br />

121<br />

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122<br />

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124<br />

124<br />

124<br />

125<br />

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126<br />

126<br />

126<br />

126<br />

126<br />

126<br />

127<br />

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20.5<br />

19.0<br />

20.7<br />

21.3<br />

20.6<br />

13.0<br />

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19.0<br />

18.0<br />

21.6<br />

21.7<br />

26.2<br />

14.0<br />

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27.8<br />

21.9<br />

20.9<br />

23.3<br />

27.9<br />

26.5<br />

26.2<br />

24.4<br />

24.8<br />

26.5<br />

28.2<br />

26.2<br />

23.9<br />

24.4<br />

21,0<br />

26.5<br />

0.8<br />

24.7<br />

23.3<br />

20.0<br />

18.0<br />

20.1<br />

22.2<br />

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35.0<br />

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26.0<br />

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41.0<br />

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61.0<br />

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64.0<br />

563.0<br />

612.0<br />

703.0<br />

730.0<br />

636.0<br />

522.0<br />

636.0<br />

571.0<br />

596.0<br />

69.0<br />

682.0<br />

644.0<br />

663.0<br />

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552.0<br />

38.0<br />

858.0<br />

667.0<br />

639.0<br />

662.0<br />

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674.0<br />

649.0<br />

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>>> H M c


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Page 21 of BURNTBUSH OVERBURDEN DRILLING >>> H M C


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1181 131<br />

1182 131<br />

1183 131<br />

1184 131<br />

1185 131<br />

1184 131<br />

1187 132<br />

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1190 132<br />

1191 132<br />

1192 132<br />

1193 132<br />

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RNTBUSH OVERBURDEN DRILLING<br />

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24.8<br />

24.1<br />

24.1<br />

21.5<br />

-0.2<br />

-0.2<br />

23.4<br />

0.3<br />

Yb<br />

-2.0<br />

33.0<br />

29.0<br />

32.0<br />

19.0<br />

28.0<br />

32.0<br />

34.0<br />

-2.0<br />

2.0<br />

34.0<br />

32.0<br />

32.0<br />

30.0<br />

33.0<br />

33.0<br />

33.0<br />

2.0<br />

3.0<br />

31.0<br />

3.0<br />

Zn<br />

150.0<br />

190.0<br />

170.0<br />

240.0<br />

210.0<br />

270.0<br />

-240.0<br />

240.0<br />

-100.0<br />

150.0<br />

-100.0<br />

-100.0<br />

170.0<br />

-100.0<br />

-100.0<br />

270.0<br />

250.0<br />

-100.0<br />

130.0<br />

120.0<br />

180.0<br />

Ce<br />

46.0<br />

904.0<br />

936.0<br />

923.0<br />

592.0<br />

569.0<br />

920.0<br />

838.0<br />

25.0<br />

25.0<br />

960.0<br />

856.0<br />

823.0<br />

818.0<br />

851.0<br />

856.0<br />

813.0<br />

29.0<br />

34.0<br />

967.0<br />

28.0<br />

NaX<br />

3.3<br />

i.O<br />

-0.9<br />

-0.9<br />

-0.9<br />

-0.7<br />

-1.4<br />

-0.9<br />

0.6<br />

1.3<br />

-0.7<br />

-0.6<br />

0.9<br />

-0.8<br />

-0.9<br />

1.1<br />

-0.8<br />

1.9<br />

3.5<br />

-0.5<br />

2.4<br />

Sn<br />

-100.0<br />

-290.0<br />

-300.0<br />

-310.0<br />

-330.0<br />

-240.0<br />

-550.0<br />

-290.0<br />

-100.0<br />

-100.0<br />

300.0<br />

-200.0<br />

-280.0<br />

-280.0<br />

-290.0<br />

-290.0<br />

-270.0<br />

-100.0<br />

-100.0<br />

220.0<br />

-100.0<br />

>>> H M c


RAPPORT: 037-6834 ( COUPLET ) INFO. DE RIFIRENCEs PO 23485<br />

CLIENT: C06EMA CANADA LTEE<br />

PROJET: 47<br />

SOUMIS PAR: JOHN LEARN<br />

DATE DE L'IMPRESSION: 23-DEC-87<br />

TYPES D'ICHANTILLONS<br />

NOMBRE<br />

FRACTION UTILISIE<br />

NOMBRE<br />

PRIP. DE L'ICHAN.<br />

NOMBRE<br />

H CONC.MINERALIX LOURDS 15<br />

2 -150 15<br />

Pulvirisation -150<br />

Enveloppage<br />

Mise en Capsules<br />

l<br />

l<br />

l<br />

REMARGUES: < MOINS QUE<br />

COPIES DU RAPPORT S: JOHN LEARN<br />

FACTURE S: JOHN LEARN<br />

RAPPORT: O37-6834<br />

PROJET: 47<br />

PABE<br />

lA<br />

NUMIRO DE<br />

L'ICHANTILLON<br />

ILIMENT<br />

UNITIS<br />

Au<br />

PPB<br />

Sb<br />

PPM<br />

As<br />

PPM<br />

Ba<br />

PPM<br />

Cd<br />

PPM<br />

Cs<br />

PPM<br />

Cr<br />

PPM<br />

Co<br />

PPM<br />

Eu<br />

PPM<br />

Hf<br />

PPM<br />

Ir<br />

PPB<br />

Fe<br />

PCT<br />

H2 BOB-87-02-09<br />

H2 BOB-87-06-02<br />

H2 BOB-87-07-05<br />

H2 BOB-87-34-12<br />

H2 BOB-87-34-15<br />

O8<br />

23<br />

622<br />

25<br />

41<br />

1.1<br />

1.7<br />

0.8<br />

0.9<br />

0.9<br />

77<br />

80<br />

39<br />

132<br />

101<br />

000<br />

OOO<br />

OOO<br />

180<br />

OOO<br />

39<br />

^7<br />

^0<br />

^8<br />

*35<br />

O<br />

o<br />

2<br />

1300<br />

1100<br />

1400<br />

1100<br />

1500<br />

140<br />

330<br />

240<br />

210<br />

89<br />

5<br />

5<br />

7<br />

5<br />

9<br />

228<br />

85<br />

293<br />

190<br />

230<br />

OOO<br />

OOO<br />

OOO<br />

000<br />

OOO<br />

23.0<br />

26.0<br />

26.0<br />

29.0<br />

26.0<br />

H2 BOB-87-58-03<br />

H2 BOB-87-64-03<br />

H2 BOB-87-74-02<br />

H2 BOB-87-86-05<br />

H2 BOB-87-89-09<br />

H2 BOB-B7--93-04<br />

H2 BOB-87-94-07<br />

H2 BOB-B7-101-14<br />

H2 BOB-87-104-18<br />

H2 BOB-B7-.17.2-05<br />

--:2i<br />

^0<br />

29<br />

59<br />

OS<br />

160<br />

180<br />

590<br />

43<br />

56<br />

0.8<br />

0.4<br />

•i0.2<br />

0.8<br />

1.7<br />

1.0<br />

0.3<br />

0.4<br />

0.5<br />

0.4<br />

14<br />

16<br />

14<br />

36<br />

498<br />

14<br />

^<br />

14<br />

52<br />

19<br />

OOO<br />

OOO<br />

000<br />

000<br />

OOO<br />

OOO<br />

000<br />

OOO<br />

OOO<br />

OOO<br />

02<br />

^9<br />

O2<br />

OO<br />

^7<br />

^8<br />

^8<br />

^4<br />

*;23<br />

^9<br />

O<br />

O<br />

O<br />

o o<br />

o o o<br />

1400<br />

1300<br />

1300<br />

1300<br />

1300<br />

1400<br />

1200<br />

1000<br />

1100<br />

1200<br />

110<br />

86<br />

62<br />

110<br />

73<br />

51<br />

67<br />

120<br />

81<br />

83<br />

9<br />

8<br />

8<br />

12<br />

6<br />

7<br />

10<br />

6<br />

6<br />

10<br />

309<br />

261<br />

242<br />

180<br />

86<br />

200<br />

297<br />

221<br />

231<br />

273<br />

OOO<br />

OOO<br />

000<br />

000<br />

OOO<br />

OOO<br />

000<br />

000<br />

OOO<br />

OOO<br />

25.0<br />

24.0<br />

21.0<br />

25.0<br />

21.0<br />

25.0<br />

24.0<br />

22.0<br />

22.0<br />

24.0


RAPPORT: 037-6834 PROJETs 47 PAGE IB<br />

NUMIRO DE<br />

L'ICHANT ILLON<br />

H2 BOB- 87-02-09<br />

H2 BOB-87-06-02<br />

H2 BOB-B7-07-05<br />

H2 BOB-87-34-12<br />

H2 BOB-87-34-15<br />

H2 BOB-87-58-03<br />

H2 BOB-87-64-03<br />

H2 BOB-87-74-02<br />

H2 BOB-87-86-05<br />

H2 BOB-87-89-09<br />

H2 BOB-87-93-04<br />

H2 BOB-87-94-07<br />

H2 BOB-87-101-14<br />

H2 BOB-87-104-18<br />

H2 BOB-87-132-05<br />

ILIMENT<br />

UNITIB<br />

La<br />

PPM<br />

340<br />

330<br />

380<br />

320<br />

702<br />

596<br />

567<br />

702<br />

470<br />

330<br />

400<br />

480<br />

330<br />

350<br />

450<br />

Mo<br />

PPM<br />

Ni<br />

PPM<br />

O 180<br />

C 6 280<br />

C6 190<br />

7<br />

^<br />

140<br />

120<br />

C 6 50<br />

C6 67<br />

C7 72<br />

C6<br />

C5<br />

73<br />

65<br />

< 5 < 50<br />

^ 60<br />

C4 110<br />

^ 50<br />

C6 83<br />


l l l l l l<br />

l<br />

I l l l l l l l l l<br />

l l<br />

Ref. No. 87-CND-47-04<br />

(Doc. #0076U)<br />

APPENDIX IV<br />

BEDROCK CHIP DESCRIPTIONS AND CHEMISTRY RESULTS<br />

- Bedrock Chip Description<br />

- Bedrock Chip Rock Geochemistry Results<br />

- Geochemistry Results from New Outcrop<br />

(sample JL-40-1)<br />

By: A. Morin<br />

J. Learn<br />

R. St-Jean<br />

January 1988


A. GREYWACKES<br />

BEDROCK CHIP DESCRIPTIONS<br />

SAMPLE if<br />

BOB-01-10<br />

BOB-02-11<br />

BOB-03-08<br />

BOB-04-05<br />

BOB-05-07<br />

BOB-06-03<br />

PURITY*<br />

At<br />

A+<br />

At<br />

B<br />

B<br />

NAME<br />

- biotite schist (BS)<br />

- BS<br />

- BS<br />

- metasediment (MS)<br />

- BS<br />

- biotite-amphibole<br />

schist (BAS)<br />

* At M no contamination scales progressively to<br />

D s very strongly contaminated<br />

COLOUR<br />

- medium grey (MG)<br />

- dark grey (DG) to<br />

black (B)<br />

- DG to B<br />

- dark green (DGN)<br />

rock chips and<br />

green clay<br />

- MG to DG<br />

- DG<br />

MINERALS<br />

- biotite (bi)<br />

- feldspar (fs)<br />

quartz (qz)<br />

- minor disseminated<br />

sulfide (dissero. sf)<br />

- bi, fs, qz<br />

- minor dissem. sf<br />

calcite* (cc)<br />

-hi<br />

- fs, qz<br />

- pyrite (py) as<br />

fracture coatings (fx)<br />

- bi, amphibole (amp)<br />

- bi, fs, qz<br />

- possible minor amp<br />

- trace chalcopyrite<br />

(cpy), py on f K<br />

- fei<br />

- fs, qz<br />

- minor amp<br />

TEXTURAL FEATURES<br />

- granolepidoblastlc<br />

- well foliated (fol'd)<br />

- fine-grained (f. gr.)<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- granolepidoblastlc<br />

- well fol'd<br />

- f. gr.<br />

- most of sample drills<br />

to clay, very few rock<br />

chips<br />

- two types of fragments<br />

one is BS, one is amp<br />

rich<br />

- moderately to well fol'd<br />

- f. gr.<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- granolepidoblastlc<br />

- well fol'd<br />

- f. gr<br />

(to be ci<br />

VEINING, ALTERATION<br />

- thin minor sterile<br />

quartz veins (q)<br />

- thin minor q with<br />

minor s f<br />

- minor chloritization<br />

(chl'n) of bi<br />

- local hematite (hem)<br />

stain<br />

- local rusty<br />

surfaces (sfc)<br />

- minor chl'n of bi<br />

- very minor q ± cc<br />

veinlng, sterile<br />

intinued )<br />

* presence of cc determined by HC1 test in field


A. CREYWACKES (cont'd)<br />

SAMPLE it<br />

BOB-07-08<br />

PURITY<br />

B<br />

- BS<br />

NAME<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

- bi, chlorite (chl)<br />

- fs, qz<br />

- possible minor amp<br />

(v.f.gr.)<br />

TEXTURAL FEATURES<br />

- granolepidoblastic<br />

- well fol'd<br />

- very fine grained<br />

VEINIKG. ALTERATION<br />

- very minor sterile<br />

milky q<br />

- strong chl'n<br />

BOB-08-03<br />

C<br />

- BS<br />

- light grey (LG)<br />

to MG<br />

-bi<br />

- fs, qz<br />

- v.f.gr.<br />

- granolepidoblastic<br />

- well fol'd<br />

- possible minor chl'n<br />

of bi<br />

BOB-09-11<br />

B<br />

- BS<br />

- DG to dark<br />

greenish grey<br />

(DOG)<br />

- fs, qz, bi<br />

- minor garnet (gt) and<br />

possibly minor amp<br />

- granolepidoblastic<br />

- well fol'd<br />

- v.f.gr.<br />

BOB-10-05<br />

B<br />

- BAS<br />

- DG<br />

- fs, qz, bi<br />

- minor amp<br />

- granoblastic<br />

- weakly fol'd<br />

- grain size variable,<br />

common coarse mica<br />

flakes (up to 1.5 cm)<br />

- minor carbonate vein,<br />

q<br />

BOB-11-02<br />

B<br />

- BS<br />

- B<br />

- fei<br />

- fs, qz<br />

- possible minor amp<br />

- granoblastic<br />

- weakly fol'd<br />

- f. gr. to v.f.gr.<br />

- minor q<br />

BOB-12-20<br />

C<br />

- MS<br />

- medium greenish<br />

grey (MGG) rock<br />

chips and green<br />

(GN) clay<br />

- fs, qz, chl<br />

- minor gt<br />

- very minor SF<br />

- very minor cc<br />

- massive<br />

- v.f.gr.<br />

BOB-13-04<br />

D<br />

- BS<br />

- DG to brownish<br />

grey<br />

- bi, fs, qz<br />

- granoblastic<br />

- weak to moderate<br />

foliation (fol'n)<br />

- minor sterile q<br />

BOB-14-03<br />

B<br />

- BS<br />

- DG to B<br />

- bi<br />

- fs, qz<br />

- possible minor amp<br />

- granolepidoblastic<br />

- minor q with minor py<br />

- well fol'd<br />

- minor green dyke or<br />

- f. gr.<br />

alteration on fx<br />

(to be c ontlnued)


A. GREYWACKES (cont'd)<br />

SAMPLE i\<br />

BOB- 15-02<br />

PURITY<br />

B<br />

- BAS<br />

NAME<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

- fei<br />

- fs, qz<br />

- minor amp<br />

TEXTURAL FEATURES<br />

- granolepidoblastic<br />

- well fol'd<br />

- weakly lineated 1<br />

- f. gr.<br />

VEINING. ALTERATION<br />

- minor sterile q<br />

BOB-16-07<br />

B<br />

- BAS<br />

- DGG<br />

-fei<br />

- fs, qz<br />

- minor amp<br />

- granoblastic<br />

- weakly fol'd<br />

- f. gr.<br />

- very minor sterile q<br />

- minor greenish mafic<br />

dyke ?<br />

BOB-17-21<br />

C<br />

- MS<br />

- DG rock chips<br />

and GN clay<br />

- fs, qz, bi<br />

- possible minor amp<br />

- very minor sf<br />

- granoblastic<br />

- weakly fol'd<br />

- f. gr.<br />

- thin mafic dykes<br />

BOB-18-06<br />

BOB-19-07<br />

C<br />

B<br />

- BAS<br />

- MS<br />

- DG to B<br />

- dark bluish grey<br />

to B<br />

-fei<br />

- fs, qz<br />

- minor amp<br />

- minor dissem. py and<br />

possibly cpy<br />

- a*<br />

- note blue qz<br />

- bi, sericite<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- minor white sterile q<br />

- sericite on altera<br />

tion ?<br />

BOB-20-16<br />

C<br />

- BAS<br />

- DG to B<br />

- fs, qz, bl<br />

- minor amp<br />

- minor dissem. py<br />

- granoblastic<br />

- weakly to moderately<br />

well fol'd<br />

- rusty surfaces (sfc)<br />

BOB-21-18<br />

B<br />

- BS<br />

- DG<br />

- fs, qz, bi<br />

- possible minor amp<br />

- a few py cubes<br />

- granoblastic<br />

- weakly to moderately<br />

well fol'd<br />

- v.f.gr. to f. gr.<br />

- minor dark green clay<br />

(mafic dykes f)<br />

BOB-22-05<br />

A<br />

- BS<br />

- B to dark brown<br />

- fs, qz<br />

- minor dissem. py<br />

-fei<br />

- well fol'd<br />

- f. gr.<br />

- granolepidoblastic<br />

- very minor q<br />

(to be c ontinued)


A. GREYWACKES (cont'd)<br />

SAMPLE i!<br />

BOB-23-13<br />

PURITY<br />

B<br />

- BS<br />

NAME<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

-bi<br />

- fa, qz<br />

- minor dissent, py<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

VEINING. ALTERATION<br />

BOB-26-24<br />

B<br />

- BS<br />

- brownish black<br />

- bi, fs, qz<br />

- minor small g t<br />

- minor cc and e f<br />

- granolepidoblastic<br />

- moderate fol'n<br />

- f .gr, with a few<br />

coarse mica flakes<br />

- minor q<br />

- minor chl in fol'n<br />

planes and/or fx and<br />

and in q<br />

BOB-27-15<br />

B<br />

- BS<br />

- dark brown<br />

- bi<br />

- fs, qz<br />

- minor dissem. py<br />

- granoblastic<br />

- massive to well fol'd<br />

- v.f.gr.<br />

- minor q with chl<br />

on vein walls<br />

BOB-28-08<br />

A<br />

- BS<br />

- DG<br />

- fei<br />

- fs, qz<br />

- minor muscovite or<br />

sericite<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- minor sterile q<br />

- sericite on<br />

alteration ?<br />

BOB-29-16<br />

C<br />

- BAS<br />

- DG to B<br />

- fs, qz, bl<br />

- note blue qz<br />

- minor amp<br />

- minor cc<br />

- granolepidoblastic<br />

- moderate fol'n<br />

- f. gr.<br />

- minor q with tourma<br />

line (tnt) py and<br />

possibly arsenopyrite<br />

- (asp)<br />

- minor cc veinlets<br />

BOB-30-21<br />

C<br />

- BAS<br />

- DGG<br />

- bi<br />

- fs, qz<br />

- minor amp<br />

- abundant dissent,<br />

euhedral py, minor cpy<br />

- granolepidoblastic<br />

- weakly fol'd<br />

- f. gr.<br />

- thin pink granite dyke<br />

- siliceous green dyke<br />

with minor sf<br />

- minor dirty q with sf<br />

(to be c ontinued )


A. GREYWACKES (cont'd)<br />

SAMPLE if<br />

BOB-31-24<br />

PURITY<br />

B<br />

- BS<br />

NAME<br />

COLOUR<br />

- DG and light<br />

greenish grey<br />

MINERALS<br />

- fs, qz, bl<br />

- some chip camples more<br />

eiliceous -* two<br />

subdivisions of BS may<br />

be present in sample<br />

- possible minor amp in<br />

more mafic chips<br />

- abundant dissem. py<br />

TEXTURAL FEATURES<br />

- granoblastic<br />

- fol'd<br />

- f.gr.<br />

VEINING, ALTERATION<br />

- q •f epidote vein<br />

with sf<br />

BOB-32-14<br />

B<br />

- BAS<br />

- DG<br />

- fs, qz, bi<br />

- minor amp<br />

- minor cc<br />

- granolepidoblastic<br />

- well fol'd<br />

- f.gr.<br />

- minor q with tm<br />

- chl'n of bl<br />

BOB-33-15<br />

A<br />

- BS<br />

- B to dark brown<br />

-fei<br />

- fs, qz<br />

- minor gt, possible<br />

minor amp<br />

- minor cc<br />

- granolepidoblastic<br />

- well fol'd<br />

- f.gr.<br />

- minor sterile q<br />

BOB-35-10<br />

D<br />

- BS<br />

- DG<br />

- fs, qz, bi<br />

- minor cc<br />

- minor magnetite (rot)<br />

- f. gr.<br />

- granoblastic<br />

- weakly to moderately<br />

well fol'd<br />

- very minor thin q<br />

BOB-36-16<br />

C<br />

- BS<br />

- DG to brown<br />

- fs, qz, bi<br />

- minor dissem. py<br />

- minor cc<br />

- minor mt<br />

- granolepidoblastic<br />

- well fol'd<br />

- f.gr.<br />

- minor q with py<br />

- minor chl'n of bi<br />

BOB-104-20<br />

B<br />

- BS<br />

- DG to B<br />

- bi, chl<br />

- qz, fs<br />

- well fol'd<br />

- f.gr.<br />

- minor q<br />

BOB-107-23<br />

B<br />

- BS<br />

- dark brown to B<br />

- bi<br />

- qz, fs<br />

- dissem. py<br />

- fol'd<br />

- f.gr.<br />

- minor q<br />

- local chl'n<br />

- carbonate on fx<br />

(to be c Dntlnued)


A. GREYUACKES (cont'd)<br />

SAMPLE tt<br />

BOB- 108-14<br />

PURITY<br />

A<br />

- BAS<br />

NAME<br />

COLOUR<br />

- dark brownish grey<br />

MINERALS<br />

- bl, qz, f e<br />

~ minor amp<br />

TEXTURAL FEATURES<br />

- moderately well fol'd<br />

- f. gr.<br />

VEINING. ALTERATION<br />

- rusty sfc<br />

BOB-109-20<br />

A<br />

- BS<br />

- brovmlsh black<br />

-fei<br />

- qz, fs<br />

- well fol'd<br />

- f. gr.<br />

- minor q<br />

BOB-110-13<br />

B<br />

- MS<br />

- dark brown to G<br />

and DGN<br />

- bl, qz, chl<br />

- amp<br />

- two rock types present,<br />

one is BS, well fol'd;<br />

other is massive amp<br />

rich<br />

- minor q<br />

- local chl'n of bl<br />

BOB-111-12<br />

BOB-112-07<br />

BOB- 113- 13<br />

A<br />

A<br />

A<br />

- BS<br />

- BS<br />

- BAS<br />

- MG<br />

- DG<br />

- MG to DG<br />

- as.<br />

~ bi, fs<br />

-ki<br />

qz, fs<br />

- as.<br />

- bi, fs<br />

- minor amp<br />

- dissem. py<br />

- fol'd<br />

- v.f.gr. to f. gr.<br />

- well fol'd<br />

- f. gr.<br />

- granoblastic<br />

- weakly fol'd<br />

- f. gr.<br />

""<br />

- local chl'n of bl<br />

BOB-114-14<br />

-15<br />

C<br />

B<br />

- BS<br />

- DG<br />

- bi<br />

- qz, fs<br />

- possible minor amp<br />

- minor dissem. py<br />

- well fol'd<br />

- f. gr.<br />

BOB-116-05<br />

A<br />

- BS<br />

- DG to B<br />

- bi, qz, fs<br />

- minor py<br />

- fol'd<br />

- f. gr. to v.f.gr.<br />

- minor q<br />

BOB-117-06<br />

A<br />

- BS<br />

- DG to brownish<br />

black<br />

- fei<br />

- qz, fs<br />

- minor gt<br />

- lepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- minor q<br />

(to be c ontinucd)


A. GREYwACKES (cont'd)<br />

SAMPLE ff<br />

BOB-118-08<br />

PURITY<br />

A+<br />

- BS<br />

NAME<br />

COLOUR<br />

- DC to brownish<br />

black<br />

MINERALS<br />

-fei<br />

- V, fs<br />

- minor py<br />

TEXTURAL FEATURES<br />

- lepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

VEINING, ALTERATION<br />

- minor q<br />

BOB-119-02<br />

A+<br />

- BS<br />

- DG to slightly<br />

g r en i eh grey<br />

- Bi, qz, fs<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- local chl'n of bi<br />

BOB-120-02<br />

C<br />

- BS<br />

- DG to B<br />

- bl, qz, fs<br />

- minor dissem. py<br />

- granolepidoblastic<br />

- moderately well fol'd<br />

- f. gr.<br />

- minor q<br />

- rusty sfc<br />

BOB-121-02<br />

A<br />

- BS<br />

- dark brownish<br />

grey to B<br />

- fei<br />

- qz, fs<br />

- minor gt<br />

- lepidoblastic<br />

- very well fol'd<br />

- f. gr.<br />

- minor q<br />

- weak chl'n<br />

BOB-122-10<br />

B<br />

- BS<br />

- DG<br />

-bl<br />

- qz, fs<br />

- lepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- minor q<br />

- carbonate on fx<br />

- local chl'n<br />

- rusty sfc<br />

BOB-123-07<br />

-08x<br />

-09x<br />

A<br />

C<br />

B<br />

- BAS<br />

- DG to B<br />

- bl, qz, fs<br />

- minor amp<br />

- interbedded amp bearing<br />

and bi-rich layers<br />

- weakly to moderately<br />

fol'd<br />

- f. gr.<br />

BOB-125A-04X<br />

C<br />

- BS<br />

- brownish black<br />

- fei<br />

- qz, fs<br />

- minor gt<br />

- lepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

- abundant q<br />

BOB-126-06<br />

C<br />

- BS<br />

- DG<br />

- bi, qz, fs<br />

- minor sf<br />

- granolepidoblastic<br />

- well fol'd<br />

- f. gr.<br />

(to be c<br />

- sterile q<br />

- rusty sfc<br />

on tinned)


A. GREYWACKES (cont'd)<br />

SAMPLE C/<br />

BOB-128-17<br />

PURITY<br />

- MS<br />

NAME<br />

"<br />

COLOUR<br />

MINERALS<br />

- bl<br />

- abundant dissem. sf<br />

TEXTURAL FEATURES<br />

- most of sample drills<br />

to clay, few rock chips<br />

VEINING. ALTERATION<br />

- abundant q<br />

BOB-129-11<br />

- MS<br />

- C<br />

- bi<br />

- dissem. sf<br />

- most of sample drills<br />

to clay, few rock chips<br />

""<br />

BOB- 130- 11<br />

B<br />

- BS<br />

- MG to DG<br />

- bi, qz, fs<br />

- diseem. py<br />

- massive to weakly fol'd<br />

- f. gr. to v.f.gr.<br />

- minor q<br />

- rusty spots<br />

x<br />

indicates sample not sent for chemistry (insufficient quantity) or too contaminated for chemistry given that<br />

good clean sample taken above or below<br />

(Document 00083U)


B. ARCILLITES<br />

SAMPLE it<br />

BOB-88-07<br />

PURITY<br />

A<br />

NAME<br />

- arsillite<br />

COLOUR<br />

- MG to DG<br />

MINERALS<br />

- abundant dissent, py<br />

TEXTURAL FEATURES<br />

- strong echlstosity/fol'n<br />

- v.f.gr. to aphanitic<br />

VEINING. ALTERATION<br />

- minor q with py, tm<br />

- rusty sfc<br />

BOB-127-21<br />

C<br />

- argillite<br />

- DG to B<br />

- v. minor sf<br />

- most of sample drills<br />

to clay, many small<br />

rock chips<br />

- v.f.gr. to aphanitic<br />

(Document C/0083U)


C. FOUR PROBLEMATIC SAMPLES FROM THE HETASEDIHENTARY TERRANE<br />

SAMPLE if \ PURITY i NAME<br />

BOB-24-18 A - BS ?<br />

Comments :<br />

High Gr, Co, Se<br />

Low La, Th, Na<br />

(relative to other greywackes)<br />

- B<br />

COLOUR<br />

MINERALS<br />

- bi, amp<br />

- fs, qz<br />

- minor gt<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- granoblastic<br />

- very weakly fol'd<br />

- f. gr.<br />

VEINING. ALTERATION<br />

- minor q<br />

- local rusty sfc<br />

BOB-25-19<br />

Comments :<br />

B<br />

High Cs, Cr, Co<br />

(relative to other greywackes)<br />

- green clay<br />

- amp f<br />

- chloritic f<br />

- most of sample drills<br />

to clay<br />

- few rock chips are<br />

fissile and friable<br />

- abundant q with<br />

rutile needles<br />

BOB-115-18<br />

Comments :<br />

Low Cs, Co, Fe, La, Se, Th<br />

(relative to other greywackes)<br />

- abundant fragments of<br />

various types, impos<br />

sible to guess if<br />

bedrock was intersected<br />

BOB-124-17<br />

Comments :<br />

Low Cs, Th<br />

(relative to other greywackes)<br />

- only rock flour was<br />

recovered, no chips<br />

(Document C/0083U)


D. HETAGABBROS<br />

SAMPLE It<br />

BOB-45-02<br />

PURITY<br />

B<br />

NAME<br />

- metagabbro (MG)<br />

COLOUR<br />

- DC and White<br />

MINERALS<br />

- amp, fs, qz<br />

- minor dissem. py<br />

- locally magnetic<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- very weakly fol'd<br />

- f. gr.<br />

- minor section drills<br />

to clay<br />

VEINING. ALTERATION<br />

- abundant q, with minor<br />

py<br />

- hem staining<br />

BOB-46-03<br />

At<br />

- MG (resembles<br />

gabbro at T3)<br />

- DC to B<br />

- amp, fs<br />

- minor py<br />

- thinly laminated<br />

(lam' d) -* sheared ?<br />

- llneated t<br />

- f, gr. to medium grained<br />

(m. gr.)<br />

- heterogranular<br />

- minor q<br />

BOB-47-07<br />

A+<br />

- MG<br />

- DGG to B<br />

- amp<br />

- bi, fs<br />

- minor dlssem. py and<br />

possibly pyrrhotite (po)<br />

- minor cc<br />

- f. gr.<br />

- minor q<br />

- chl on fx<br />

BOB-48-01<br />

-02<br />

A<br />

B4-<br />

- MG<br />

- DG to B (01)<br />

- DGG (02)<br />

~ USE<br />

- fs<br />

- dlssem. py, cpy<br />

- locally magnetic<br />

- minor cc<br />

- massive to weakly fol'd<br />

(wrinkly)<br />

- lineated<br />

- White q, with coarse<br />

muscovite flakes<br />

(s3 mm)<br />

- rusty sfc<br />

- hem staining<br />

- thin sf velnlets<br />

- thin cc veinlets<br />

BOB-55-08<br />

A<br />

- MG<br />

- DG to DGN<br />

- amp<br />

- fs<br />

- magnetic<br />

- minor cc<br />

- moderate fol'n<br />

- f. gr.<br />

- chl present<br />

- hem stain<br />

BOB-57-03<br />

A<br />

- MG<br />

- DGG to B<br />

- amp, fs<br />

- minor cc<br />

- massive to weakly fol'd<br />

- f. gr. to v.f.gr.<br />

- minor sterile q<br />

- LG to MG felsic dyke<br />

- rusty sfc<br />

(to be c ontinued)


D. HETAGABBROS (cont'd)<br />

SAMPLE #<br />

BOB-59-06<br />

PURITY<br />

B<br />

- MO<br />

NAME<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

- amp<br />

- interlayers (veins f)<br />

of qz<br />

- minor dlssem. py, cpy<br />

- locally magnetic<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- schistose (sheared f)<br />

- linea ted f<br />

- f. gr.<br />

VEINING. ALTERATION<br />

- minor sterile q<br />

BOB-60-05<br />

B<br />

- MG<br />

- DC to B and White<br />

- amp<br />

- fs<br />

- dlssem. sf<br />

- minor cc<br />

- locally magnetic<br />

- massive<br />

- f. gr. granular<br />

- q 4- carbonate veins<br />

BOB-64-04<br />

A+<br />

- MG<br />

- DG to B<br />

- clay is GK<br />

- amp<br />

- blue qz (rounded<br />

dlssem. grains)<br />

- minor dlssem. py<br />

- strongly magnetic (po)<br />

- equigranular<br />

- massive<br />

- f. gr. to m. gr.<br />

- some of sample drilled<br />

to rock flour clay<br />

- py on fx<br />

- hem staining<br />

BOB-69-01<br />

A+<br />

- MG<br />

- MG to B<br />

- bl, amp, fs, qz<br />

- dlssem. py and probably<br />

also cpy<br />

- locally magnetic<br />

- equigranular<br />

- weakly fol'd<br />

- f. gr. to m. gr.<br />

- minor q (white to<br />

yellow)<br />

- hem stain<br />

- rusty sfc<br />

BOB- 70-03<br />

A<br />

- MG<br />

- DG to B<br />

- amp, bl, fs<br />

- dlssem. py<br />

- equigranular<br />

- massive to moderately<br />

fol'd<br />

- weakly lineated<br />

- f. gr.<br />

- rusty sfc<br />

BOB- 7 2-04<br />

A+<br />

- MG<br />

- DG to bluish green<br />

- amp<br />

- fs<br />

- minor cc<br />

- massive to well fol'd<br />

(sheared t)<br />

- f. gr.<br />

(to be c<br />

- minor q<br />

- chl'd<br />

ontinued)


D. HETAGABBROS (cont'd)<br />

SAMPLE 0<br />

BOB-91-08<br />

PURITY<br />

A<br />

- MG<br />

KAME<br />

COLOUR<br />

- B to DGN<br />

MINERALS<br />

- amp, bl (f)<br />

- fs<br />

- minor dissem. Bf<br />

TEXTURAL FEATURES<br />

- massive<br />

- weakly lineated<br />

- f. gr. to m. gr.<br />

VEINING. ALTERATION<br />

- carbonate on fx<br />

- rusty spots<br />

BOB-93-07<br />

A<br />

- MG<br />

- DGN<br />

- amp, fs<br />

- locally well developed<br />

lineation<br />

- minor q<br />

- rusty spots<br />

BOB-95-06<br />

B<br />

- MG<br />

- DGG<br />

- amp, fs<br />

- minor py<br />

- massive to weakly<br />

lineated (?)<br />

- f .gr. to m. gr.<br />

- minor q<br />

BOB-97-17<br />

A<br />

- MG<br />

- DGN<br />

- amp, fs<br />

- dissem. py<br />

- strongly magnetic (mt)<br />

- massive<br />

- coarse grained<br />

BOB-102-14<br />

A<br />

- MG<br />

- DGG to B<br />

- amp<br />

- fs<br />

- minor actinolite<br />

- massive<br />

- f. gr.<br />

- rusty sfc<br />

- local chl'n<br />

BOB- 103- 18<br />

A<br />

- MG<br />

- B<br />

- amp, fs<br />

- dissem. py<br />

- massive<br />

- f. gr. to m. gr.<br />

- epidote on fx<br />

BOB-105-09<br />

B<br />

- MG<br />

- DG to B<br />

- amp, bi, fs<br />

- minor actinolite<br />

- massive to weakly<br />

lineated<br />

- f. gr. to m. gr.<br />

- minor q<br />

- rusty sfc<br />

BOB-131-08<br />

-09<br />

A<br />

B<br />

- MG<br />

- DGG to B (08)<br />

- dark browlsh grey<br />

to B and DGN<br />

- amp, fs<br />

- weakly magnetic (po)<br />

- massive<br />

- v.f.gr. to f. gr. to<br />

m. gr.<br />

- abundant q 4- carbonate<br />

veins (08)<br />

- rusty spots<br />

BOB- 132-08<br />

-09<br />

B<br />

A<br />

- MG<br />

- DG to B (08)<br />

- dark to medium<br />

green (09)<br />

- amp<br />

- fs<br />

- locally magnetic (po)<br />

- massive<br />

- f. gr.<br />

- minor q and/or carbo<br />

nate veins<br />

- epidote veinlets<br />

- rusty spots and sfcs<br />

(to be c ontinued)


D. HETAGABBROS (cont'd)<br />

SAMPLE it<br />

BOB- 133-02<br />

-03x<br />

PURITY<br />

A<br />

B<br />

- MG<br />

NAME<br />

COLOUR<br />

- greenish black<br />

MINERALS<br />

- amp<br />

- (s<br />

- locally masnetlc (po)<br />

TEXTURAL FEATURES<br />

- massive<br />

- weakly llneated<br />

- f.sr.<br />

VEINING, ALTERATION<br />

- rusty spots (02)<br />

- abundant q, carbonate<br />

veinlets (03)<br />

(Document 00083U)


E. MAFIC TO INTERMEDIATE VOLCANICS<br />

(distinguished in part using lithogeochemistry results)<br />

SAMPLE if<br />

BOB-40-01<br />

PURITY<br />

A<br />

NAME<br />

- qz eye tuff<br />

COLOUR<br />

- medium to DGG<br />

MINERALS<br />

- fs, qz, amp<br />

- strongly magnetic (mt)<br />

- dissem. py<br />

TEXTURAL FEATURES<br />

- weakly fol'd<br />

- f. gr. to m.gr.-<br />

VEINING. ALTERATION<br />

BOB-41-06<br />

B<br />

- intermediate C int.)<br />

ash tuff<br />

- DGG<br />

- fs, qz, bi<br />

- possible minor<br />

amp, chl<br />

- minor dissem. py<br />

- magnetic<br />

- minor cc<br />

- well fol'd<br />

- f.gr.<br />

- minor sterile q<br />

BOB-42-09<br />

C<br />

- ash tuff and/or<br />

MG (probably two<br />

rock types)<br />

- DO to brown<br />

- amp<br />

- bl, chl<br />

- massive to well fol'd<br />

- f.gr.<br />

- minor q<br />

BOB-49-05<br />

C<br />

- felsic to int. tuff<br />

- medium green<br />

- fs, amp<br />

- minor py, cpy<br />

- locally magnetic<br />

- pervasive minor cc<br />

- equigranular<br />

- massive to thinly lam' d<br />

- v.f.gr.<br />

- minor q with s f<br />

- rusty sfc<br />

BOB-50-01<br />

B<br />

- int. tuff<br />

- IXJ and white<br />

- amp porphyroblasts (f)<br />

- very minor qz eyes<br />

- dissem. py<br />

- strongly magnetic<br />

- pervasive minor cc '<br />

- massive to fol'd<br />

- f.gr. to med.gr.<br />

- abundant q with sf<br />

- also q * cc veinlets<br />

- rusty spots<br />

BOB-51-03<br />

B<br />

- felsic tuff<br />

- light yellowish<br />

greenish<br />

- siliceous<br />

- abundant dissem. py<br />

some cpy<br />

- locally magnetic<br />

- equigranular<br />

- thinly lam'd (sheared?)<br />

- v.f.gr.<br />

- minor q with py,<br />

possibly asp<br />

- rusty sfc<br />

BOB-51-04<br />

A<br />

- garnetiferous tuff<br />

- medium to DGG<br />

- amp, fs, bi<br />

- minor gt Kl mm)<br />

- minor dissem. py, cpy<br />

- strongly magnetic<br />

- thinly lam'd<br />

- v.f.gr.<br />

- chl'n of bi (?)<br />

- very minor q<br />

(to be c antinued)


E. MAFIC TO INTERMEDIATE VOLCANICS (cont'd)<br />

(distinguished in part using lithogeochemistry results)<br />

SAMPLE it<br />

BOB-52-03<br />

PURITY<br />

B<br />

NAME<br />

- int. tuff<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

- amp, fs<br />

- minor gt, tm<br />

- minor dissent, py<br />

- strongly magnetic, lo<br />

cally pervasive minor cc<br />

TEXTURAL FEATURES<br />

- thinly lam' d<br />

- v.f.gr. to f. gr.<br />

VEINIHG. ALTERATION<br />

- minor q<br />

- minor thin pale green<br />

veinlets (epidote t)<br />

BOB-58-04<br />

B<br />

- int. tuff ?<br />

- brownish black<br />

chips<br />

- greenish clay<br />

- minor py, cpy aggre<br />

gates<br />

- minor cc<br />

- much of bedrock drills<br />

to clay, soft rock<br />

- strongly fractured,<br />

sheared f<br />

- massive<br />

- v.f.gr.<br />

- q with tm<br />

- oxidized fx sfc<br />

BOB-62-12<br />

- int. tuff ?<br />

- dark green to<br />

B chips<br />

- greenish clay<br />

- altered bi<br />

- most of bedrock drills<br />

to clay<br />

- fol'd<br />

- f. gr.<br />

- minor q<br />

BOB-63-02<br />

C<br />

- int. flow or<br />

ash tuff<br />

- DG to B<br />

- amp, fs<br />

- dissem. py<br />

- minor cc<br />

- locally magnetic<br />

- massive, speckled<br />

- f. gr.<br />

- minor q<br />

- carbonate on fx<br />

BOB-65-05<br />

C<br />

- int. tuff ?<br />

- DG to B<br />

- amp, bl, fs<br />

- dissem. py<br />

- moderately magnetic<br />

- weakly fol'd<br />

- f .gr. to m. gr.<br />

- minor q-fs veins<br />

- hem. stain<br />

- rusty sfc<br />

BOB-67-08<br />

B<br />

- int. flow or<br />

ash tuff<br />

- DG to B<br />

- amp, bi<br />

- heulandite crystals f?<br />

- dissem. and patchy py<br />

- minor cc<br />

- speckled<br />

- well fol'd<br />

- f. gr.<br />

- rusty sfc<br />

BOB-68-01<br />

A<br />

- int. flow or<br />

ash tuff<br />

- PG to B<br />

- amp, bi, chl, fs<br />

- dissem. py<br />

- strongly magnetic<br />

- equigranular<br />

- moderate fol'n<br />

- f .gr. to m. gr.<br />

- white q<br />

(to be c antinued)


E. MAFIC TO INTERMEDIATE VOLCANICS (cont'd)<br />

(distinguished in part using lithogeochemistry results)<br />

SAMPLE tt<br />

BOB-74-03<br />

PURITY<br />

C<br />

NAME<br />

- garnetiferous tuff<br />

COLOUR<br />

- DG to B<br />

MINERALS<br />

- amp, bl, f e<br />

- minor gt<br />

- abundant dissem. py<br />

and possibly cpy<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- equigranular<br />

- fol'd, locally massive<br />

- f .gr. to m. gr.<br />

VEINING. ALTERATION<br />

- q<br />

BOB-86 -06<br />

A<br />

- garnetiferous tuff<br />

- medium greenish<br />

grey to DG<br />

- minor gt<br />

- minor py<br />

- porphyroblastic<br />

- fol'd<br />

- f. gr.<br />

BOB-87-04<br />

A<br />

- int. tuff<br />

- MG to DG<br />

- amp, bi, fs<br />

- minor gt t<br />

- minor dissem. py<br />

- equigranular<br />

- fol'd<br />

- f.gr.<br />

- minor q with py<br />

- rusty sfc<br />

BOB-89-11<br />

B<br />

- int. tuff<br />

- DG<br />

- dissem. py<br />

- magnetic (mt)<br />

- fol'd<br />

- f.gr.<br />

- minor q<br />

- locally rusty sfc<br />

BOB-92-04<br />

B<br />

- garnetiferous tuff<br />

- DG and brown<br />

- minor gt<br />

- slightly magnetic (Mt)<br />

- heulandite ?f<br />

- massive<br />

- f.gr. to v.f.gr.<br />

- py in fx abundant<br />

- rusty spots and sfc<br />

BOB-94-08<br />

B<br />

- int. flow<br />

- DGG<br />

- dissem. py<br />

- weakly magnetic<br />

- massive<br />

- f.gr. to m. gr.<br />

- minor q with tm<br />

- minor carbonate in fx<br />

- rusty sfc<br />

BOB-96-17<br />

A<br />

- qz eye tuff<br />

- MG and white<br />

- minor qz eye (O mm)<br />

- abundant py<br />

- locally magnetic<br />

- heulandite tt<br />

- weakly fol'd<br />

- f.gr.<br />

- abundant q<br />

- rusty spots and sfc<br />

(to be c ontinued)


E. MAFIC TO INTERMEDIATE VOLCANICS (cont'd)<br />

(distinguished in part using lithogeochemistry results)<br />

SAMPLE if<br />

BOB-98-13<br />

PURITY<br />

C<br />

NAME<br />

- fs crystal tuff<br />

COLOUR<br />

- light green to<br />

medium greenish<br />

grey<br />

MINERALS<br />

- abundant fs<br />

phenocryste (O mm)<br />

- minor garnet<br />

- minor dissem py/po<br />

TEXTURAL FEATURES<br />

- porphyritic<br />

- fol'd (bedded f)<br />

- f. gr. to v.f.gr.<br />

VEINING. ALTERATION<br />

BOB-99-05<br />

A<br />

- int. tuff<br />

- DGG<br />

- strongly magnetic (mt)<br />

- fol'd<br />

- f. gr.<br />

- minor q<br />

BOB-100-19<br />

A<br />

- int. flow or tuff<br />

- DG to B<br />

- weakly fol'd<br />

- f, gr. to v.f.gr.<br />

- epidote/carbonate<br />

on fx<br />

- minor q<br />

- rusty sfc<br />

(Document 00083U)


F. FELSIC TO INTERMEDIATE METAVOLCANIC ROCKS<br />

SAMPLE it<br />

BOB-76-01<br />

PURITX<br />

At<br />

NAME<br />

- felsic crystal tuff<br />

COLOUR<br />

- medium pink to red<br />

MINERALS<br />

- abundant round qz eyes<br />

(O mm)<br />

- fs phenocrysts<br />

- mafic minerals in small<br />

localized patches eg<br />

bi, amp<br />

- abundant dissent, py,<br />

possibly also asp<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- porphyritic, aphanitic<br />

- weakly fol'd to massive<br />

VEINING. ALTERATION<br />

- minor q<br />

- minor green mafic<br />

dykes<br />

BOB-78-06<br />

BOB-79-03<br />

A<br />

A<br />

- felsic crystal tuff<br />

- felsic crystal tuff<br />

- bronish red<br />

- medium red to<br />

brownish red<br />

- Is<br />

- minor round qz eyes<br />

(


F. FELSIC TO INTERMEDIATE HETAVOLCANIC ROCKS (eont'd)<br />

SAMPLE f<br />

BOB-77-03<br />

PURITY<br />

B<br />

NAME<br />

- felsic tuff<br />

COLOUR<br />

- MGG with occa<br />

sional black<br />

layers<br />

MINERALS<br />

- fs phenocrysts and<br />

qz eyes present but not<br />

abundant<br />

- dominantly qz, fs<br />

- abundant dissem. py<br />

- minor cc<br />

- locally magnetic<br />

TEXTURAL FEATURES<br />

- weakly porphyritic<br />

- v.f.gr. siliceous<br />

groundmass<br />

- layered, f di 'd<br />

- weakly sheared ?<br />

VEINING. ALTERATION<br />

- abundant q<br />

- epidote veinlets<br />

- rusty fx<br />

BOB-77-04<br />

B<br />

- felsic tuff<br />

- MGG<br />

- as above with abundant<br />

dissem. py<br />

- thinly lam 1 d<br />

- abundant q<br />

BOB-82-13<br />

A<br />

- felsic tuff<br />

- MG and light<br />

greenish grey<br />

- elongate fs phenocrysts<br />

- fs, qz, bl<br />

- dissem. py<br />

- minor cc<br />

- strongly magnetic (m t)<br />

- weakly porphyritic<br />

- v.f.gr. to aphanitic<br />

groundmass<br />

- minor q<br />

- rusty fx<br />

BOB-85-10<br />

A<br />

- felsic tuff<br />

- light green and MG<br />

- few fs phenocrysts<br />

- fs, qz, bl<br />

- minor dissem. py<br />

- minor cc<br />

- locally magnetic<br />

- weakly porphyritic<br />

- v.f.gr. siliceous<br />

groundmass<br />

- fol'd (sheared f)<br />

- minor fuchsite<br />

staining<br />

BOB-43-08<br />

B<br />

- Intermediate (Int.)<br />

tuff<br />

- DG to brown with<br />

minor light<br />

greenish clay<br />

(rock flour)<br />

- minor dissem. py<br />

- minor cc<br />

- locally magnetic<br />

- well fol'd to massive<br />

- sugary but f .gr. to<br />

v.f.gr.<br />

- minor q<br />

- rusty/hem staining<br />

- cc restricted to fx f<br />

BOB-44-01<br />

B<br />

- felsic tuff<br />

- MG to B<br />

- siliceous<br />

- abundant dissem. py<br />

- minor cc<br />

- strongly magnetic<br />

- massive<br />

- v.f.gr.<br />

- minor q with py<br />

- rusty sfc<br />

(to be contlnued)


F. FELSIC TO INTERMEDIATE METAVOLCANIC ROCKS (cont'd)<br />

SAMPLE #<br />

BOB-80-02<br />

PURITY<br />

A<br />

NAHG<br />

- felsic tuff<br />

COLOUR<br />

- MG and white<br />

MINERALS<br />

- siliceous, brittle<br />

- fs, bi, sericite<br />

- abundant dissem. py<br />

- strongly magnetic<br />

(dissem. mt)<br />

TEXTURAL FEATURES<br />

- fol'd (sheared f)<br />

- f. gr. to v.f.gr.<br />

equigranular<br />

VEINING. ALTERATION<br />

- abundant sterile q<br />

- rusty spots<br />

- sericite on<br />

alteration f<br />

BOB-84-08<br />

B<br />

- felsic tuff<br />

- MG to DG locally<br />

LG and light green<br />

- siliceous<br />

- dissem. rounded blue qz<br />

- py In patches<br />

- minor cc<br />

- magnetic (mt)<br />

- thinly lam' d, layered<br />

- fol'd<br />

- v.f.gr.<br />

- fuchsite staining<br />

- locally rusty<br />

BOB-38-17<br />

A<br />

- qz eye tuff<br />

- DGG<br />

- elongate qz eyes<br />

abundant<br />

- fs, bi, note blue qz<br />

- dissem. py<br />

- locally magnetic<br />

- porphyritic<br />

- well fol'd<br />

- v.f.gr. to f. gr.<br />

BOB-39-21<br />

- DG clay, few rock<br />

chips<br />

- rock chips of various<br />

lithologles, diffi<br />

cult to guess bedrock<br />

BOB-53-02<br />

A<br />

- felsic tuff t<br />

- LG<br />

- siliceous<br />

- minor dissem. py<br />

- massive<br />

- lam' d T<br />

- f. gr. to v.f.gr.<br />

- minor q f<br />

- rusty sfc<br />

BOB-54-04<br />

A+<br />

- felsic tuff ?<br />

- LG to white<br />

- siliceous<br />

- minor dissem. py<br />

- locally weakly magnetic<br />

- massive<br />

- bedded ?<br />

- f. gr.<br />

- chl t<br />

- hem. staining<br />

- limonite sfc<br />

(to be c* jntlnued)


F. FELSIC TO INTERMEDIATE METAVOLCAHIC ROCKS (cont'd)<br />

SAMPLE tt<br />

BOB-56-04<br />

-05<br />

PURITY<br />

C<br />

B<br />

NAME<br />

- felsic tuff<br />

- DGG<br />

COLOUR<br />

MINERALS<br />

- abundant rounded qz eyes<br />

- discern, blue qz<br />

- fs<br />

- amp f<br />

- minor py, cpy<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- porphyritic<br />

- moderately to well fol'd,<br />

locally massive<br />

- f. gr. to m. gr.<br />

VEINIHG. ALTERATION<br />

- abundant thin<br />

sterile q<br />

BOB-61-14<br />

C<br />

- felsic tuff<br />

- medium greenish<br />

grey<br />

- siliceous<br />

- 3 mm bi flakes<br />

- fine py crystals<br />

- minor cc<br />

- massive to weakly fol'd<br />

- f. gr.<br />

- thin chl-muscoviteqz-fs<br />

dyke<br />

- hem staining<br />

BOB-66-02<br />

B<br />

- fs crystal tuff<br />

- MG to B<br />

- abundant fs phenocryst B<br />

(laths to 3 mm)<br />

- minor qz eyes<br />

- amp, bi<br />

- very minor ef , possibly<br />

po (locally magnetic)<br />

- minor cc<br />

- porphyritic<br />

- thinly lam' d<br />

- groundmass v.f.gr.<br />

- minor q with tm<br />

BOB-71-01<br />

At<br />

- fs crystal tuff<br />

- B and white<br />

- rich in fs, qz<br />

- bi, amp<br />

- minor dlssem. py<br />

possibly also asp<br />

- minor cc<br />

- may be very strongly<br />

porphyritic, but fs is<br />

subhedral to anhedral<br />

suggesting intrusive<br />

rock<br />

- coarse grained 1-5 mm<br />

- hem staining<br />

BOB- 73-02<br />

A<br />

- felsic flow or tuff<br />

- MG to DG<br />

- fs phenocrysts (O mm)<br />

- amp laths J<br />

- fs, bi, qz<br />

- porphyritic<br />

- minor grey q<br />

- amygdular f<br />

- weakly fol'd<br />

- f. gr. groundmass<br />

- part of sample drilled<br />

to rock flour clay<br />

(to be c ontinued)


F. FELSIC TO INTERMEDIATE HETAVOLCANIC ROCKS (cont'd)<br />

SAMPLE 0<br />

BOB-75-01<br />

PURITY<br />

C<br />

NAME<br />

- qz eye tuff or<br />

felsic flow<br />

COLOUR<br />

- DG to MG<br />

MINERALS<br />

- fs, bi, amp, qz<br />

- qz eyes or amysdales 7<br />

- minor cc<br />

TEXTURAL FEATURES<br />

- fol'd, possibly<br />

flattened<br />

- f.sr.<br />

VEINING. ALTERATION<br />

- carbonate veinlet<br />

- py in schistosity<br />

BOB-90-15<br />

B<br />

- Int. flow<br />

- DG and medium to<br />

dark green<br />

- dissent, py crystals<br />

- locally masnetic<br />

- massive<br />

- v.f.gr.<br />

- hem staining<br />

- rusty<br />

BOB-101-16<br />

B<br />

- felsic tuff<br />

- light green to<br />

medium yellowish<br />

brown<br />

- granular<br />

- weakly fol'd<br />

- v.f.gr.<br />

- soft, drills to clay<br />

- carbonate on fx<br />

- strongly altered<br />

(Document #008311)


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Pige<br />

Record<br />

229<br />

230<br />

231<br />

232<br />

233<br />

234<br />

235<br />

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238<br />

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240<br />

241<br />

242<br />

243<br />

244<br />

245<br />

246<br />

247<br />

248<br />

249<br />

250<br />

251<br />

252<br />

253<br />

254<br />

255<br />

254<br />

257<br />

258<br />

259<br />

. 260<br />

261<br />

" 262<br />

243<br />

. 244<br />

245<br />

246<br />

247<br />

248<br />

249<br />

270<br />

271<br />

272<br />

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274<br />

275<br />

276<br />

277<br />

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279<br />

280<br />

281<br />

282<br />

283<br />

1 t<br />

St<br />

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2<br />

3<br />

4<br />

5<br />

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7<br />

8<br />

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51<br />

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54<br />

55<br />

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WEATHER LOG<br />

As has been done in the past, a weather log is<br />

included for interest only.


•**"*^. \<br />

ilCOGEMA<br />

PICHE DE TEMPERATURE<br />

DATE<br />

24/02<br />

25/02<br />

26/02<br />

27/02<br />

28/02<br />

01/03<br />

02/03<br />

03/03<br />

04/03<br />

05/03<br />

06/03<br />

HEURE<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

^vT-<br />

/X^x<br />

X<br />

X<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

i^xx<br />

C— < — *^y<br />

x<br />

x<br />

x<br />

c^s<br />

C--O-— '<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

sn Vv V<br />

? vs * * * *<br />

# ^ #<br />

* * * *<br />

* * *<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

MAX,<br />

-2<br />

*3<br />

48<br />

MIN.<br />

REMARQUES<br />

les temperatures viennent du camp<br />

Newmont<br />

very light snow, but it is colder<br />

strong wind, cold<br />

accumulation overnight -8 cm<br />

total accum. *20-25 cm<br />

wet snow<br />

Doc. //0027U<br />

Piche 0TMP-2


Canada<br />

Ltde/Ltd.<br />

PICHE DE TEMPERATURE<br />

DATE<br />

07/03<br />

08/03<br />

09/03<br />

10/03<br />

11/03<br />

12/03<br />

13/03<br />

14/03<br />

15/03<br />

16/03<br />

17/03<br />

HEURE<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

^t:<br />

X^-r-'N<br />

X<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

)^5<br />

^— "C-^V-X<br />

x<br />

J^-\<br />

c^X./-— '<br />

X<br />

X<br />

X<br />

f'/'/<br />

'/'s s/<br />

f V /<br />

* * * *<br />

* * * *<br />

# ^ *<br />

* * tt<br />

x<br />

x<br />

x<br />

MAX. MIN. REMARQUES<br />

V<br />

very warm today<br />

very light snow, no accumulation<br />

very light snow, no accumulation<br />

very cold this morning<br />

extremely cold *-25 OC ?<br />

cold nights, warm days<br />

eg *-200C, -2 0C<br />

,, full moon<br />

Doc. #0027U<br />

Piche flTMP-2


Canada<br />

Lt^e/Ltd.<br />

PICHE DE TEMPERATURE<br />

DATE<br />

18/03<br />

19/03<br />

20/03<br />

21/03<br />

22/03<br />

23/03<br />

24/03<br />

25/03<br />

26/03<br />

27/03<br />

28/03<br />

HEURE<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

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18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

^( * * r—<br />

X<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

fe*g^<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

's'/'/ //^ f'//<br />

x<br />

* * * *<br />

* * * *<br />

*"\<br />

\<br />

MAX. MIN. REMARQUES<br />

Timmins broke record for light temp.<br />

for this day 22/3; today 160C, pre<br />

vious record 1919 at 130C<br />

rain after 9 pm<br />

foggy<br />

very minor light snow on ground<br />

very minor light snow on ground<br />

light rain all day<br />

Doc. //0027U<br />

Piche f/TMP-2


FICHE DE TEMPERATURE<br />

DATE<br />

29/03<br />

30/03<br />

31/03<br />

01/04<br />

02/04<br />

03/04<br />

04/04<br />

05/04<br />

06/04<br />

HEURE<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

08 h<br />

18 h<br />

18 h<br />

^V^L<br />

/S-r-X^<br />

X<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

x<br />

^^ ^— C.A-V<br />

x<br />

x<br />

x<br />

x<br />

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c-^O^<br />

x<br />

x<br />

x<br />

x<br />

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# * # *<br />

* * * *<br />

u<br />

Jt<br />

^f V S<br />

x<br />

x<br />

x<br />

x<br />

x<br />

MAX, MIN. REMARQUES<br />

accum. -10 cm<br />

Doc. //0027U<br />

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Canada<br />

Ltfc/Ltd.<br />

PICHE DE TEMPERATURE<br />

DATE<br />

03/06<br />

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Doc. #0027U<br />

HEURE<br />

•~\ * * r~"<br />

/S-^S<br />

AM<br />

AM/PM<br />

PM<br />

AM<br />

soir<br />

AM/PM<br />

AM<br />

AM/PM<br />

AM/PM<br />

AM/PM<br />

AM/PM<br />

AM/PM<br />

AM/PM<br />

AM/PM<br />

AM<br />

AM<br />

^xx<br />

^— 4 — X-V<br />

PM<br />

PM<br />

AM/PM<br />

AM/PM<br />

PM<br />

PM<br />

AM<br />

PM<br />

PM<br />

AM<br />

PM<br />

PM<br />

^r-s<br />

C^O-—'<br />

AM<br />

PM/nuit<br />

AM<br />

PM<br />

AM<br />

PM<br />

PM<br />

f'/'/<br />

'/'s V<br />

t v s<br />

nuit<br />

nuit<br />

nuit<br />

AM<br />

nuit<br />

mid i<br />

nuit<br />

AM tot<br />

PM<br />

PM<br />

* ***<br />

*<br />

#<br />

*<br />

^<br />

*<br />

*<br />

*<br />

* * w<br />

MAX. MIN. REMARQUES<br />

matin pluvieux (frais)<br />

matin frais (fumge)<br />

matin frais; plusieurs averses PM<br />

thunder showers<br />

thunder showers<br />

Fiche 0TMP-2


:V, S/'<br />

Canada<br />

Ltfc/Ltd.<br />

PICHE DE TEMPERATURE<br />

DATE<br />

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HEURE<br />

-~\ * * r~~<br />

/ST-'N<br />

AM<br />

AM<br />

AM<br />

PM<br />

AM<br />

PM<br />

AM<br />

AM<br />

AM<br />

AM<br />

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N — K — X-X<br />

PM<br />

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AM<br />

PM<br />

PM<br />

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AM<br />

PM<br />

PM<br />

AM<br />

PM<br />

PM<br />

PM<br />

PM<br />

PM<br />

PM<br />

AM<br />

e^r\<br />

c— 'C/-—<br />

PM<br />

PM<br />

PM<br />

PM<br />

AM<br />

PM<br />

AM<br />

AM<br />

AM<br />

AM<br />

AM/PM<br />

AM/PM<br />

AM<br />

/s'/'/ SH<br />

f'//<br />

AM<br />

PM<br />

so ir<br />

AM<br />

PM<br />

nuit<br />

AM<br />

soir/nuii<br />

soir/nui<br />

* * * *<br />

* * * #<br />

*<br />

* jt<br />

*<br />

*<br />

*<br />

MAX. MIN. REMARQUES<br />

thunder showers<br />

thunder showers<br />

thunder showers<br />

morning fog<br />

t<br />

steady heavy rain all night - minor<br />

thunder lightning " "<br />

Doc. //0027U<br />

Piche f/TMP-2


NOSEWORTHY TP<br />

HURTUBI^E^TP<br />

i ~^<br />

\ Alt<br />

\<br />

79040<br />

49035<br />

Biotite schist<br />

Felsic crystal tuffs<br />

Felsic to intermediate metavolcanics<br />

Mafic to intermediate metavolcanics<br />

GEOCHEMISTRY SYMBOLS<br />

5-9 ppb Au<br />

A I0-19ppb Au<br />

A ^20 ppb Au<br />

x Q Outcrop<br />

Strike and dip of foliation<br />

Azimuth and plunge of minor fold axis<br />

Diamond drill hole, inclined<br />

(drilled by previous claimholders<br />

Reverse circulation drill hole<br />

Outcrops referred to in text<br />

3C 30' ?90OO'<br />

16 13<br />

XKIEMA Canada<br />

Ltee/Ltd.<br />

SCALE: h 1/20,000<br />

12<br />

14 15<br />

INDEX TO ADJOINING<br />

N.T.S. SHEETS<br />

l 7 50,000<br />

10<br />

2000 2500<br />

4CHJO 6000 BOOO<br />

BURNTBUSH RIVER PROJECT<br />

GEOLOGY AND GOLD GEOCHEMISTRY OF<br />

BEDROCK CHIP SAMPLES FROM<br />

REVERSE CIRCULATION DRILLING<br />

c^<br />

Interpretation by: J. Learn, A. j<br />

Drofted by: R. Allie li *"'<br />

Bose mop:<br />

Revise by:<br />

1/88<br />

8/86<br />

Annex no.<br />

MAP NO. 10<br />

5<br />

HOBLITZELU TP<br />

NOSEWORTHY TP<br />

Metagrabbro<br />

.MG A-MG A.FV<br />

l \ l<br />

32E12Sffeiai4 63.5467 NOSEWORTHY<br />

\<br />

200 \<br />

HOBLITZELL<br />

TOMLINSO'N<br />

r\ ,<br />

nF<br />

Nr<br />

/rarin<br />

Dote<br />

r<br />

Report no-87-CND-47-04


490 32 — 49032'<br />

73 574 000 m E 79 040<br />

NOSEWORTHY<br />

HURTUBISE<br />

——rv/ ^ ——<br />

35'<br />

Meters 300<br />

ij<br />

SCALE; l: 1/20,000<br />

16<br />

D<br />

-J.OLJ-<br />

Hcn<br />

8<br />

1<br />

13<br />

12<br />

'<br />

2<br />

-1 'f.<br />

t<br />

14<br />

II<br />

3? P- ^jc. t.<br />

6<br />

1 —————<br />

1 ' •S<br />

INDEX TO ADJOINING<br />

Canada<br />

Ltce/Ltd.<br />

J<br />

N.T.S. SHEETS<br />

l X 50,00C<br />

IOLO iroo 2000 2500<br />

•K-OO BOCO<br />

BURNTBUSH RIVER PROJECT<br />

Interpretation by; J. Learn<br />

prof ted by: R AII le<br />

Base map:<br />

Revise by:<br />

LOCATION OF DRILL HOLES<br />

AND KEY TO SECTIONS<br />

Dote<br />

12/87<br />

8/86<br />

15<br />

10<br />

Report no.87-CND-47-04<br />

Annex no.<br />

MAP NO. l<br />

7<br />

2<br />

490 35<br />

\ HOBLITZELL TP NOSEWORTHY TP<br />

49030<br />

BOB-6H BCB-64\<br />

49027 -<br />

HOBLITZELL<br />

TOMLINSO'N


LEGEND<br />

—— APPROXIMATE LIMIT OF CLEARED AREA<br />

APPROXIMATE LIMIT OF MECHANICAL STRIPPING<br />

WATER FILLED DEPRESSION<br />

5m. x 5rn. SQUARES, NUMBERED AND<br />

INDIVIDUALLY MAPPED<br />

INDEX MAP<br />

SCALE: 1/500<br />

O 5 10m.<br />

l l______l<br />

100m due North<br />

to A<br />

N<br />

3C faO"00 50 790 00' 30<br />

———————<br />

LEGEND<br />

16<br />

13<br />

14<br />

15<br />

9<br />

12<br />

li<br />

10<br />

-4.O U.<br />

*TC. n<br />

* ————<br />

32 F-<br />

\Jfrn 1——<br />

PRINCIPAL ROCK TYPES:<br />

Acid tuff or rhyolite<br />

Iron rich tuffs (lapilli to agglomerate).<br />

SYMBOLS:<br />

40<br />

Geologic contact, observed<br />

Strike and dip of foliation (and bedding)<br />

8<br />

1<br />

5<br />

o<br />

* i<br />

o<br />

6<br />

o w<br />

m 3<br />

•Ul<br />

3<br />

j<br />

INDEX TO ADJOINING<br />

N.T.S.<br />

SHEETS<br />

l/ 50,000<br />

7<br />

2<br />

Dacltlc tuff<br />

Mixed tuffs (iron rich and dacitlc tuffs)<br />

LATE DYKE AND VEIN<br />

Diabase dyke<br />

Ouartz-epldote (-chlorite) veins ^ segregations<br />

20<br />

Azimuth and plunge of minor fold axis<br />

Strike and dip of veins, vertical dip, dip direction<br />

\ \\ known but not measured<br />

y//<br />

X T5-2<br />

Strike and approximate dip of discrete fractures,<br />

vertical, inclined<br />

Sense of movement<br />

Orientation of glacial striae, ice direction inferred<br />

from regional knowledge<br />

Sample location<br />

BLOZEC LINE E -W CLAIM!<br />

POET l<br />

Northern section<br />

Scale X 100<br />

'anadn<br />

lee/Ltd.<br />

BURNTBUSH RIVER PROJECT<br />

8m,<br />

-305 63,5V67<br />

Quartz, quartz-epldote veins<br />

l GC003<br />

Channel sample location<br />

Limit of outcrop<br />

TRENCH 5<br />

TRENCH 5<br />

DETAILED GEOLOGIC MAP<br />

Epidote veinlets<br />

Water or overburden filled depression in outcrop<br />

exposure<br />

( Southern section )<br />

B:<br />

Southern sedion<br />

Interpretation by: A. Morin ^LuxJU<br />

Dale<br />

Report no. 67-CND-47-06<br />

32E12SW00I4 63.5467 NOSEWORTHY<br />

SCALE- 1/2000<br />

n 20 40m<br />

l_____l_____i<br />

Drafted by: R Allie 19/8/87<br />

Base map:<br />

Revise by:<br />

Annex no.<br />

MAP NO.


INDEX MAP<br />

---. BLAZED CLAIM LINE<br />

—— — APPROXIMATE LIMIT OF CLEARED AREA<br />

APPROXIMATE<br />

LIMIT OF MECHANICAL STRIPPING<br />

WATER<br />

FILLED DEPRESSION<br />

5m x 5m. SQUARES, NUMBERED AND INDIVIDUALLY MAPPED<br />

5 - 10 ppb Au<br />

- 20 ppb Au<br />

>ZO ppb Au<br />

SCALE :IX500<br />

O 5 lOm<br />

^-^Xs^<br />

\ 0<br />

LEGEND<br />

PRINCIPAL ROCK TYPES:<br />

Acid ruff or rhyolite<br />

Iron rich tuffs (lapilli to agglomerate)<br />

Dacltlc tuff<br />

Mixed tuffs (Iron rich and dacitic tuffs)<br />

LATE DYKE AND VEIN<br />

Diabase dyke<br />

Quartz-epldote (-chlorite) veins. fc segregations<br />

Quartz, quartz-epldote veins<br />

Epidote velnlets<br />

X<br />

GC002<br />

SYMBOLS:<br />

^ _.— Geologic contact, observed<br />

Strike and dip of foliation (and bedding)<br />

Azimuth and plunge of minor fold axis<br />

Strike and dip of veins, vertical dip, dip direction<br />

known but not measured<br />

'**J<br />

^ ^ Strike and approximate dip of discrete fractures,<br />

vertical. Inclined<br />

Sense of movement<br />

Orientation of glacial striae. Ice direction inferred<br />

from regional knowledge<br />

X T5-2 Sample location<br />

f GC003 Channel sample location<br />

Limit of outcrop<br />

Water or overburden filled depression in outcrop<br />

INDEX TO ADJOINING<br />

N.T.S. SHEETS<br />

l/ 50,000<br />

( V W 1 1/A 1 \ Canada<br />

V A R UJ.MALtee/Ltd.<br />

Scale: 1/100<br />

BURNTBUSH RIVER PROJECT<br />

TRENCH 5<br />

DETAILED GEOLOGIC<br />

Northern section<br />

MAP<br />

Interpretation byA.Morin<br />

Report no,R7-CND-47-06<br />

MAP NO.


^/^i's^^^yiV-^<br />

'IT' 'X' 1 t ' ' v 'i L v/ 1<br />

^^V^'xO^-0-V<br />

AAAAAAAAAAAA<br />

3ppb 5ppb<br />

4ppb<br />

NE<br />

(m.)<br />

290<br />

- 280<br />

- 260<br />

- 250<br />

- 240<br />

- 230<br />

LEGEND SYMBOLS<br />

COCHRANE TILL (and sediments)<br />

Gravel rich till<br />

(result of erosion of Oflbway II esker)<br />

OJIBWAY II SEDIMENTS<br />

5c Glaciolacustrine clay member<br />

5b Glaciolacustrine sand member (fine sands)<br />

5a Glaciofluvial member (coarse sand and gravel)<br />

Note: members may be mixed and/or Interbedded<br />

MATHESON TILL<br />

Very clayey till<br />

Very sandy till, or sandy, gravelly till<br />

Minor pure clay, sorted sandy or gravel sections<br />

MISSINAIBI SEDIMENTS<br />

3c Glaciolacustrine (clay and/or fine sand) member<br />

3a Fluvial member (coarse sand and/or gravel]<br />

Note: members may be mixed and/or Interbedded<br />

LOWER TILL<br />

Very clayey till<br />

Minor sorted gravel section<br />

OLDER SEDIMENTS ?<br />

* Quaternary stratigraphy presented Is field Interpretation; see text.<br />

T<br />

l Om<br />

HORIZONTAL SCALE l: 500O<br />

VERTICAL SCALE l: 500<br />

VERTICAL EXAGGERATION IOX<br />

2ppb<br />

Drill hole number<br />

Trace of drill hole<br />

Overburden sample with no<br />

gold grains<br />

Boulder which was sampled<br />

(mineralization present)<br />

Sample with one gold or a In<br />

Interval not sampled (clay, boulder etc.<br />

Overburden sample with 3 gold groins<br />

Bedrock surface<br />

Bedrock sample with Au result<br />

COGEMA CANADA LTD<br />

BURNTBUSH RIVER PROJECT<br />

QUATERNARY SECTION<br />

A-A1<br />

Interpretation: j. Learn, R. 1987<br />

Report no; 87-CM D-47-04 : 2<br />

SW<br />

ORGANICS<br />

A1<br />

(m)<br />

290 -<br />

22<br />

280 -<br />

270 -<br />

260 -<br />

250 -<br />


•v'— ^ ^ l' 1 ./, J PH<br />

r/ /x'W-l -'xX/^MxT/<br />

' - v' X'---- \. .-\-S.''<br />

^/rxV\V^<br />

9ppb<br />

B<br />

NE<br />

(m.)<br />

- 290<br />

- 280<br />

- 270<br />

- 260<br />

- 250<br />

- 240<br />

- 230<br />

LEGEND SYMBOLS<br />

ORGANICS<br />

COCHRANE TILL (and sediments)<br />

Gravel rich fill<br />

(result of erosion of O Jib w ay esker)<br />

OJIBWAY II SEDIMENTS<br />

5c Glaciolocustrlne clay member<br />

5b Glaciolacustrine sand member (fine sands)<br />

5o Glaciofluvial member (coarse sand and gravel)<br />

Note: members may be mixed and/or Interbedded<br />

MATHESON TILL<br />

Very clayey till<br />

Very sandy till, or sandy, gravelly till<br />

Minor pure clay, sorted sandy or gravel sections<br />

MISSINAIBI SEDIMENTS<br />

3c Glaciolacustrine (clay and/or fine sand) member<br />

3a Fluvial member (coarse sand and/or gravel)<br />

Note: members may be mixed and/or interbedded<br />

LOWER TILL<br />

^'<br />

O O Q,0<br />

(TO o* O<br />

Very clayey till<br />

OLDER SEDIMENTS ?<br />

Minor sorted gravel section<br />

t Quaternary stratigraphy presented Is field Interpretation; see text.<br />

T<br />

10m<br />

HORIZONTAL SCALE l: 5000<br />

VERTICAL SCALE l: 500<br />

VERTICAL EXAGGERATION IOX<br />

2ppb<br />

Trace of drill hole<br />

Overburden sample with no<br />

gold grains<br />

Boulder which was sampled<br />

'mineralization present)<br />

Sample with one gold grain<br />

Interval not sampled (clay, boulder etc-)<br />

Overburden sample with 3 gold grains<br />

Bedrock surface<br />

Bedrock sample with Au result<br />

COGEMA CANADA LTD<br />

BURNTBUSH RIVER PROJECT<br />

QUATERNARY SECTION<br />

8 " B '<br />

Interpretation: J. Learn, R.at-Jean 1987<br />

Report no; 87-CND-47-04 MAP: 3<br />

SW<br />

Drill hole number<br />

B'<br />

(m.)<br />

290 -<br />

280 -<br />

99<br />

270 -<br />

260 -<br />

250 -<br />

240 -<br />

230 -<br />

32E12SW0ai4 63.5467 NOSEWORTHY<br />

250


Burntbush<br />

River<br />

"*. "o"*'.". ** o o o 10<br />

\ "I . l Oo 0*0*00 Vo o" O 00<br />

Co'..'^6;''c7^<br />

3ppb<br />

3ppb<br />

10<br />

8<br />

6ppb<br />

NE<br />

- 290<br />

- 280<br />

- 270<br />

- 260<br />

- 250<br />

- 240<br />

- 230<br />

COCHRANE TILL land sediments!<br />

EL<br />

Grovel rich till<br />

(result of erosion of OJIbway II esker)<br />

OJIBWAY II SEDIMENTS<br />

5c Glaciolacustrine clay member<br />

5b Glaciolacustrine sand member (fine sands)<br />

5a Glaciofluvial member (coarse sand and gravel)<br />

Note: members may be mixed and/or Interbedded<br />

MATHESON TILL<br />

Very clayey till<br />

Very sandy till, or sandy, gravelly till<br />

Minor pure clay, sorted sandy or gravel sections<br />

MISSINAIBI SEDIMENTS<br />

3c Glaciolacustrine (clay and/or fine sand) member<br />

3a Fluvial member [coarse sand and/or grovel)<br />

Note: members may be mixed and/or Interbedded<br />

LOWER TILL<br />

Very clayey till<br />

OLDER SEDIMENTS l<br />

Minor sorted gravel section<br />

* Quaternary stratigraphy presented ts field Interpretation; see text.<br />

lOOrn—^1<br />

t<br />

l Om<br />

HORIZONTAL SCALE l: 50OO<br />

VERTICAL SCALE l: 500<br />

VERTICAL EXAGGERATION IOX<br />

2ppb'<br />

Drill hole number<br />

Trace of drill hole<br />

Overburden sample with no<br />

gold grains<br />

Boulder which was sampled<br />

(mineralization present)<br />

Sample with one gold grain<br />

Interval not sampled (clay, boulder etcj<br />

Overburden sample with 3 gold grains<br />

Bedrock surface<br />

Bedrock sample with Au result<br />

COGEMA CANADA LTD<br />

BURNTBUSH RIVER PROJECT<br />

QUATERNARY SECTION<br />

Interpretation: Jl^earn, R.St-Jean 1987<br />

Report no. 87-CND-47-04____ [MAP: 4<br />

sw<br />

LEGEND SYMBOLS<br />

ORGANICS<br />

C1<br />

290 -<br />

280 -<br />

270 -<br />

260 -<br />

250 -<br />

240 -<br />

230 -<br />

32E12SW0014 63.5467 NOSEWORTHY<br />

260


|A-^ ^M^i^^r^^^W^<br />

, .<br />

^.nv.-^i.c,.-^ .-.-^V-i^'.-.K-.-l^aJ^-— -^NE^7.--... —— --——^^^-^<br />


AAAAAAAAAAAAAAAA AAAAA<br />

lOppb<br />

46<br />

45<br />

44<br />

i^yjjji^f^s^mj^^ 106 107<br />

I4ppb R<br />

6ppb<br />

8ppb<br />

105<br />

Burntbush<br />

River<br />


I2ppb<br />

59 58<br />

AAAAAAAAAAAAAA<br />

"Tvf^vV^^V-/<br />

' l -~ ^^-"^oC'/ovTr,^;rT^v:;'j-<br />

t- X M -; ^y--, s- ^ ^<br />

X'* x " v ^ ^ ' i- C"" 1' * '^J M' y*^ ^y<br />

\^ \^ 1 ^ ' ~" V"^/ ^<br />

IT. J -^ ' L s iVi ' x '- /"'' "~ v T<br />

* — ~"~ ~ i i i -~' j. i ^<br />

3lppb<br />

A 4<br />

AAAAAAM TT J l j i i i-<br />

A A A A A A A A A A A<br />

A *<br />

n i-i 1-ij-ij-LffV^*"**"'Mr*''*"<br />

^<br />

n.nnmumjimum-yrA A A<br />

A A A A A A A<br />

4ppb<br />

Burntbush<br />

River,<br />

9C<br />

- 25C<br />

- 240<br />

LEGEND<br />

ORGANICS<br />

COCHRANE TILL (and sediments)<br />

Grovel rich till<br />

(result of erosion of Ojlbway II esker)<br />

OJIBWAY II SEDIMENTS<br />

5c Glaciolacustrine clay member<br />

5b Glaciolacustrine sand member (fine sands)<br />

5a Glaciofluvial member (coarse sand and gravel)<br />

Note: members may be mixed and/or interbedded<br />

MATHESON TILL<br />

Very clayey till<br />

Very sandy till, or sandy, gravelly till<br />

Minor pure clay, sorted sandy or gravel sections<br />

MISSINAIBI SEDIMENTS<br />

3c Glaciolacustrine (clay and/or fine sand) member<br />

3o Fluvial member (coarse sand and/or gravel)<br />

Note: members may be mixed and/or interbedded<br />

LOWER TILL<br />

Very clayey till<br />

?-!?.0'S OLDER SEDIMENTS ?<br />

Minor sorted gravel section<br />

* Quaternary stratigraphy presented Is field Interpretation; see text.<br />

10m<br />

j,<br />

HORIZONTAL SCALE l: 5000<br />

VERTICAL SCALE l: 500<br />

VERTICAL EXAGGERATION IOX<br />

2ppb<br />

SYMBOLS<br />

Drill hole number<br />

Trace of drill hole<br />

Overburden sample with no<br />

gold groins<br />

Boulder which was sampled<br />

'mineralization present)<br />

Sample with one gold grain<br />

Interval not sampled (clay, boulder etc.<br />

Overburden sample with 3 gold grains<br />

Bedrock surface<br />

Bedrock sample with Au result<br />

3. 5 V6 7<br />

COGEMA CANADA LTD<br />

BURNTBUSH RIVER PROJECT<br />

QUATERNARY SECTION<br />

F- F 1<br />

Interpretation: |^arn, R. St-Jean 1987<br />

Report no: 87^CND-47-04_____[MAP: 7<br />

w<br />

(m.)<br />

290<br />

280 -<br />


I3ppb<br />

3ppb<br />

93 94<br />

95<br />

3ppb<br />

Burntbush<br />

River<br />

- 270<br />

- 250<br />

- 240<br />

- 230<br />

COCHRANE TILL (and sediments)<br />

Gravel rich III!<br />

(result of erosion of Ojlbway II esker]<br />

OJIBWAY II SEDIMENTS<br />

5c Glaciolacustrine clay member<br />

5b Glaciolacustrine sand member [fine sands)<br />

5a Glaciofluvial member (coarse sand and gravel)<br />

Note: members may be mixed and/or Interbedded<br />

MATHESON TILL<br />

Very clayey till<br />

Very sandy till, or sandy, gravelly till<br />

Minor pure clay, sorted sandy or gravel sections<br />

MISSINAIBI SEDIMENTS<br />

3c Glaciolacustrine (clay and/or fine sand) member<br />

3a Fluvial member (coarse sand and/or gravel)<br />

Note: members may be mixed and/or Interbedded<br />

LOWER TILL<br />

Very clayey till<br />

Minor sorted gravel section<br />

OLDER SEDIMENTS ?<br />

* Quaternary stratigraphy presented Is field Interpretation; see text.<br />

T<br />

I0m<br />

HORIZONTAL SCALE l: 5000<br />

VERTICAL SCALE l: 500<br />

VERTICAL EXAGGERATION IOX<br />

2ppb<br />

Trace of drill hole<br />

Overburden sample with no<br />

gold grains<br />

Boulder which was sampled<br />

{mineralization present)<br />

Sample with one gold groin<br />

Interval not sampled (cloy, boulder etcj<br />

Overburden sample with 3 gold grains<br />

Bedrock surface<br />

Bedrock sample with Au result<br />

COGEMA CANADA LTD<br />

BURNTBUSH RIVER PROJECT<br />

QUATERNARY SECTION<br />

-G 1<br />

Interpretation: J. Learnj, ft St-Jean 1987<br />

Report no: 87-CND-47-04 MAP: 8<br />

w<br />

LEGEND SYMBOLS<br />

ORGANICS<br />

Drill hole number<br />

6'<br />

290 -<br />

3ppb<br />

280 -<br />

270 -<br />

260 -<br />

250 -<br />

240 -<br />

230 -<br />

32E12SW0014 E3.54B7 NOSEWORTHV<br />

300


SW<br />

J'<br />

123 Blue<br />

Lake 120 119 115 116<br />

VAAAAAAAAAAAA/<br />

2ppb<br />

NE SW NE<br />

H H<br />

6ppb<br />

2ppb<br />

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