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References

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234

la Sample catalogue
Appendix 1
Ib Salnple locations in the study region
le Sample locations outside of the study region
Id Location of samples collected for fluid inclusion analysis.

Appendix 1a Catalogue of representative Tawallah Group samples collected during this study.
Field No. Fm. Area Section/sample location (AMG) m Sedimentary facies or rock type Preparations
94-88 PIn Tawallah Range 5780E 82090N - 5783E 82071 N 23.5 Planar cross-bedded gravelly sandstone R,TS
94-89 PIn Tawallah Range 5780E 82090N - 5783E 82071 N 49 Planar cross-bedded sandstone R, TS
94-51 ptn Scrutton Range 5638E 82090N - 5633E 82086N 1.5 Upper planar cross-bedded sandstone R,TS
94-52 Ptn Scrutton Range 5638E 82090N - 5633E 82086N 1.5 Upper planar cross-bedded sandstone R,TS
94-53 Ptn Scrutton Range 5638E 82090N - 5633E 82086N 55 Upper ripple/aminated sandstone R,TS
94-15 PIn Batten Range 5813E 81909N - 5812E 81916N 130 Planar cross-bedded sandstone R,TS
94-14 PIn Batten Range 5813E 81909N - 5812E 81916N 166 Upper ripple laminated sandstone R, TS
94-13 PIn Batten Range 5813E 81909N - 5812E 81916N 187 Upper planar cross-bedded sandstone R,TS
94-12 Pin Batten Range 5813E 81909N - 5812E 81916N 187 Upper planar cross-bedded sandstone R, TS
94-110a Pin Batten Range 5784E 81960N Palaeosol horizon R, TS
94-110b PIn Batten Range 5784E 81960N Palaeosol horizon R,TS
92-M01 Pie Mallapunyah 5895E 81215N Coherent dolerite R,TS
92-M01 PIe Mallapunyah 5895E 81215N Coherent dolerite R,TS
92-M02 PIe Mallapunyah 5895E 81215N Coherent dolerite R,TS
92-M02 PIe Mallapunyah 5895E 81215N Coherent dolerite R, TS
92-M02 PIe Mallapunyah 5895E 81215N Coherent dolerite R, TS
93-69 PIe Serutton Range 5264E 82093N Coherent dolerite R,PO
93-71 PIe Serutton Range 5264E 82093N Coherent dolerite R, PS, PO
93-72 PIe Serutton Range 5264E 82093N Coherent dolerite R,PO
93-73 PIe Serutton Range 5264E 82093N Do omite/dolomitic siltstone R,TS,PS,PD
93-74 PIe Serutton Range 5264E 82093N Dolomite/dolomitic siltstone R, TS, PO
93-78 PIe Serutton Range 5264E 82093N Coherent dolerite R, PO
93-79 Pte Serutton Range 5264E 82093N Coherent dolerite R, PO
93-80 PIe Seruttan Range 5264E 82093N Coherent dolerite R, PS, PO
93-81 PIe Scrutton Range 5632E 82086N Coherent dolerite R,PO
93-82 PIe Scrutton Range 5632E 82086N Coherent dolerite R,PD
93-88A PIe Serutton Range 5632E 82086N Coherent dolerite R, PS, PO
93-886 PIe Scrutton Range 5632E 82086N Coherent dolerite R,PD
94-540 PIe Serutton Range 5632E 82086N Dolomite/dolomitie siltstone R, TS
94-54b PIe Scrutton Range 5632E 82086N Dolomite/dolomitic siltstane R, TS
94-58a Pte Seruttan Range 5632E 82086N Dolomite/dolomitie siltstone R, TS
94-58b Pte Scrutton Range 5632E 82086N Dolomlte/dolomitic siltstone R, TS
94-99 PIe Kiana 5246E 81320N 174.9 Coherent dolerite R,PO
94-100 PIe Kiana 5246E 81320N 169.1 Coherent dolerite R, PS, PO
94-101 PIe Kiana 5246E 81320N 166.5 Coherent dolerite R
94-104 PIe Kiana 5246E 81320N 143.9 In situ dalerite breeeia R
94-27a Plo Scrutton Range 5621E 82083N - 5618E 82081N 9.5 Carbonate association R,TS
94-27b Plo Scrutton Range 5621E 82083N - 5618E 82081N 9.5 Carbonate association R, TS
94-28 Plo Scrutton Range 5621E 82083N - 5618E 82081N 9.5 Carbonate association R, TS
94-29 Plo Scrutton Range 5621E 82083N -5618E 82081N 14.5 Sandstone association R,PS
94-30 Pto Serutton Range 5621E 82083N - 5618E 82081N 14.5 Sandstone association R, PS
94-32 Plo Scrutton Range 5621E 82083N -5618E 82081N 138 Sandstone association R,TS
94-105 Plo Masterton Horst 6206E 81756N Carbonate association R,TS
94-106 Plo Masterton Horst 6206E 81756N Carbonate association R,TS
92-M03 PIg Mallapunyah 5886E 81218N Coherent dolerite R,TS
92-M04 PIg Mallapunyah 5886E 81218N Coherent dorerite R, TS
93-90 PIg Seruttan Range 5617E 82077N Volcanic Breeeia R, TS, PS
93-99 PIg Scruttan Range 5617E 82077N Volcanic Breccia R, TS
93-107 PIg Scrutton Range 5617E 82077N Volcanic Breccia R, PS
93-108 PIg Scrutton Range 5617E 82077N Coherent dolerite R,TS
93-109 PIg Serutlan Range 5617E 82077N Volcanic Breeela R,TS
93-122 PIg Scrulton Range 5617E 82077N Volcanic Breccia R, PS
94-33a PIg Scrutton Range 5637E 82067N - 5632E 62065N 15 Sandstone R,TS
94-33b PIg Scrutton Range 5637E 82067N - 5632E 82065N 15 Sandstone R,TS
94-34 PIg Scrutton Range 5637E 82067N - 5632E 82065N 32 Coherent dolerite R,TS
94-35 PIg Scrutton Range 5637E 82067N - 5632E 82065N 32 Coherent dolerite R,PO
94-36 PIg Scrutton Range 5637E 82067N - 5632E 82065N 32 Coherent dorerite R,PO
94-37 PIg Scrutton Range 5637E 82067N - 5632E 82065N 32 Coherent dolerite R, PS, PO
94-38 PIg Serutton Range 5637E 82067N - 5632E 82065N 88 Coherent dolerite R, PO
94-39 Ptg Scrutlon Range 5637E 82067N - 5632E 82065N 88 Coherent dolerite R, PO
94-40 Ptg Serutton Range 5637E 82067N - 5632E 82065N 193 Coherent dolerite R, PO
94-41 Ptg Serutton Range 5637E 82067N - 5632E 82065N 193 Coherent dolerite R,PO
94-42 PIg Scrutton Range 5637E 82067N - 5632E 82065N 193 Coherent dolente R, PS, PO
94-43 PIg Scrutton Range 5637E 82067N - 5632E 82065N 224 Coherent dolerite R,PO
94-44 PIg Scrutton Range 5637E 82067N - 5632E 82065N 224 Coherent dorerite R, PO
94-45 PIg Scrutton Range 5637E 82067N - 5632E 82065N 253 Sandstone R, TS
94-49 PIg Scruttan Range 5637E 82067N - 5632E 82065N 228 Coherent dolerite (vesicular) R, TS
94-50 PIg Scrutton Range 5637E 82067N - 5632E 82065N 228 Coherent dolerite (vesicular) R, TS

Appendix 2
2a Inverse palaeostress analysis of fault-slip data (Batten Range)
2b Inverse palaeostress analysis offauIt-slip data (Scrutton Range)
2c Inverse palaeostress analysis of fault-slip data (Scrutton Range)

Appendix 2a
Batten Range: Lower Tawallah Group: E-W Compression
79 81 N 20 W 0 1 46 41 S 21 E 0 12 23 34 E 72 E R 23
24 63 W 46 W 0 2 67 84 S 5 W 0 13 44 27 E 40 E S 24
61 68 N 3 E 0 3 120 20 S 89 E R 14 71 32 S 0 E S 25
60 89 N 10 W 0 4 116 38 E 90 E R 15 180 74 W 18 S S 26
71 47 S 15 E 0 5 20 58 E 90 E R 16 67 46 S 8 W S 27
41 89 W 50 W 0 6 23 79 w 80 W N 17 102 20 S 11 W S 28
44 49 W 53 W 0 7 108 39 N 70 W N 18 133 44 N 32 W S 29
56 24 N 42 W 0 8 66 11 N 65 W N 19 121 31 N 14 W S 30
71 77 N 17 E 0 9 10 56 E 70 W R 20 163 84 W 18 E S 31
38 52 W 20 W 0 10 11 86 E 90 E R 21
62 45 N 11 W 0 11 34 56 E 71 E R 22
MINIMISATION PERCENT 80 SELECTED PARAMETERS, SrGMA 1 TRE=lOO PLUN= 3
LEAST SQUARE REGRESSION OF THE 24 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 21. 39169 ERROR IN R .38E+OO
NO STRESS VALUES USED AND PRINCIPAL AXES
3 3
.1 3 3
33
-
--­
3­
1 3
3 3 1.
2
2
2
2 .2
2 ...
. 2
2
2 2
*
1
3
1
111+.
3 1 +++
1+
11.
3 1
1..
2

Bat ten Range: Basal Tawallah Group - NW-SE Compression
143 77 E 45 E D 1 38 52 W 20 W D 18 23 34 E 72 E R 35
141 71 E 0 E D 2 62 45 N 11 W D 19 50 88 S 23 E S 36
70 20 S 38 E D 3 112 71 N 12 W D 20 52 83 S 3 W S 37
145 20 W 0 E D 4 46 41 S 21 E D 21 44 27 E 40 E S 38
79 81 N 20 W D 5 67 84 S 5 W D 22 71 32 S 0 E S 39
24 63 W 46 W D 6 120 20 S 89 E R 23 180 74 W 18 S S 40
119 22 S 5 W D 7 164 21 E 90 E R 24 54 70 S 12 E S 41
101 27 S 0 E D 8 176 38 E 90 E R 25 42 45 E 5 W S 42
61 68 N 3 E D 9 20 58 E 90 E R 26 37 74 E 25 E S 43
162 67 W 12 E D 10 23 79 W 80 W N 27 55 72 S 23 E S 44
150 87 W 23 E D 11 18 45 W 50 W N 28 40 66 E 15 W S 45
60 89 N 10 W D 12 108 39 N 70 W N 29 67 46 S 8 W S 46
71 47 S 15 E D 13 66 11 N 65 W N 30 102 20 S 11 W S 47
41 89 W 50 W D 14 10 56 E 70 W R 31 133 44 N 32 W S 48
44 49 W 53 W D 15 11 86 E 90 E R 32 121 31 N 14 W S 49
56 24 N 42 W D 16 34 56 E 71 E R 33 3 61 W 0 E S 50
71 77 N 17 E D 17 61 68 N 70 E R 34 163 84 W 18 E S 51
MINIMISATION PERCENT 40 SELECTED PARAMETERS, SIGMA 1 TRE=l75 PLUN= 1
LEAST SQUARE REGRESSION OF THE 20 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 21. 96397 ERROR IN R .32E+00
NO STRESS VALUES USED AND PRINCIPAL AXES STRESS RATIO R = .61
SIGMA(l)= .46252 TREND 357.0 (ERR 21.4) PLUNGE 3.0 (ERR 16.51
SIGMA(2)= .07495 TREND 261. 6 (ERR 47.01 PLUNGE 61. 5 (ERR 9.9l
SIGMA(3l= -.53748 TREND 88.6 (ERR 18.1) PLUNGE 28.3 (ERR 10.2)
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 7 36 20 43 10 50 41 24
2 .1 .2 10 11 42 7
3 .2 .3 12 44 1
4 .3 .4 14 3 37
5 .4 .5 16 28 2
6 .5 .6 18 8 4
7 .6 .7 19 45
8 .7 .8 20 34
9 .8 .9 20
10 .9 1.0 20
11 1.0 1.2 21 30
12 1.2 1.4 23 46 13
13 1.4 1. 6 24 23
14 1.6 1.8 25 40
15 1.8 2.0 31 14 35 49 39 27 38
16 2.0 2.2 34 15 5 6
17 2.2 2.4 38 21 33 31 26
18 2.4 2.6 43 16 19 32 47 12
19 2.6 2.8 47 18 9 51 29
20 2.8 3.0 50 22 17 48
21 3.0 3.2 51 25
SCHMIDT NET OF NEAREST EXACT SOLN
1
..... +.
+++ 1
+1 1
1
3
3
2 3 3
3 3
2 2 3
2 .2 • ---3
...2
3
2 3 3
2
2
1
1 1
....... .. 1 ....
1
1

Batten Range: Basal Tawallah Group: NE-SW Compression
143 77 E 45 E D 1 157 63 E 90 E R 51
141 71 E 0 E D 2 164 21 E 90 E R 52
28 66 E 37 E D 3 176 38 E 90 E R 53
45 69 S 41 W D 4 20 58 E 90 E R 54
70 20 S 38 E D 5 157 22 E 60 W R 55
14 69 E 21 W D 6 23 79 W 80 W N 56
147 21 E 50 W D 7 18 45 W 50 W N 57
145 20 W 0 E D 8 136 13 E 61 W R 58
161 71 E 5 W D 9 108 39 N 70 W N 59
79 81 N 20 W D 10 66 11 N 65 W N 60
24 63 W 46 W D 11 10 56 E 70 W R 61
119 22 S 5 W D 12 134 40 N 60 E R 62
101 27 S 0 E D 13 11 86 E 90 E R 63.
170 51 W 45 E D 14 34 56 E 71 E R 64
13 63 W 30 W D 15 61 68 N 70 E R 65
49 86 N 5 E D 16 23 34 E 72 E R 66
157 74 E 10 W D 17 50 88 S 23 E S 67
61 68 N 3 E D 18 52 83 S 3 w S 68
164 81 E 0 E D 19 44 27 E 40 E S 69
166 62 E 5 W D 20 71 32 S 0 E S 70
175 62 W 25 E D 21 180 74 W 18 S S 71
162 67 W 12 E D 22 54 70 S 12 E S 72
150 87 W 23 E D 23 42 45 E 5 W S 73
60 89 N 10 W D 24 37 74 E 25 E S 74
166 74 E 14 E D 25 125 78 N 32 W S 75
71 47 S 15 E D 26 55 72 S 23 E S 76
41 89 W 50 W D 27 93 74 S 5 E S 77
44 49 W 53 W D 28 40 66 E 15 W S 78
171 62 E 13 W D 29 80 68 S 12 E S 79
56 24 N 42 W D 30 67 46 S 8 W S 80
46 79 S 12 E D 31 102 20 S 11 W S 81
158 82 E 16 E D 32 116 61 N 10 W S 82
56 78 S 11 E D 33 88 67 S 3 E s 83
25 55 W 16 E D 34 133 44 N 32 W S 84
15 82 E 38 E D 35 161 45 W 45 W S 85
156 82 E 15 W D 36 120 89 N 5 W S 86
167 73 E 4 W D 37 129 68 S 24 W S 87
156 73 E 10 W D 38 108 88 N 28 W S 88
161 64 E 13 w D 39 121 31 N 14 W S 89
41 70 E 37 E D 40 121 54 S 30 w S 90
71 77 N 17 E D 41 3 61 W 0 E S 91
159 73 E 14 W D 42 112 59 S 12 W S 92
38 52 W 20 W D 43 101 81 N 3 E S 93
161 63 E 10 W D 44 114 63 N 15 E S 94
168 74 E 14 W D 45 127 59 N 5 E S 95
62 45 N 11 W D 46 115 71 N 4 E S 96
112 71 N 12 W D 47 113 42 N 13 E S 97
46 41 S 21 E D 48 123 24 S 0 E S 98
67 84 S 5 W D 49 131 36 s 10 E S 99
120 20 S 89 E R 50 136 39 W 21 W S 100
168 35 W 40 W S 101
163 84 W 18 E S 102
MINIMISATION PERCENT 50 SELECTED PARAMETERS, SIGMA 1 TRE=225 PLUN=15 LEAST
SQUARE REGRESSION OF THE 51 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 21.67805 ERROR IN R .39E+OO
NO STRESS VALUES USED AND PRINCIPAL AXES\
SIGMA(I)= .45043 TREND 241.1 (ERR 13.2) PLUNGE 12.7 (ERR 15.7)
SIGMA(2)= .09915 TREND 115.1 (ERR 43.9) PLUNGE 69.0 (ERR 17.4)
SIGMA(3)= -.54957 TREND 334.9 (ERR 11.7) PLUNGE 16.4 (ERR 15.2)
STRESS RATIO R = .65
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 16 100 87 83 45 62 19 31 95 82 92 58 21 79 29 42 33
2 .1 .2 22 88 7 32 34 37 17
3 .2 .3 31 97 98 75 38 9 39 86 77 90
4 .3 .4 37 55 20 14 44 99 96
5 .4 .5 39 6 25
6 .5 .6 45 93 85 36 94 35 4
7 .6 .7 49 16 15 101 3
8 .7 .8 50 40
9 .8 .9 51 51
10 .9 1.0 51
11 1.0 1.2 59 81 89 52 22 48 59 11 43
12 1.2 1.4 61 53 27
13 1.4 1.6 69 84 24 63 56 64 18 66 70
14 1.6 1.8 74 54 69 41 23 80
15 1.8 2.0 78 60 61 46 50
16 2.0 2.2 84 28 26 49 57 1 5
17 2.2 2.4 84
18 2.4 2.6 86 13 76
19 2.6 2.8 93 73 68 10 72 12 74 30
20 2.8 3.0 100 65 102 91 71 67 8 47
21 3.0 3.2 102 78 2

SCHMIDT NET OF NEAREST EXACT SOLN
3
.. 33 3 3 3
.3.3-333
3 3---3 3
3 3­
3
3 3 3
2 2
2 2
22 2
* 2 22 22
2 ... 22
1 2 222.2 2
2 2
1 1
1 2
11 +1 11 1
+++1111
11+
1
1 11
1..
1
2 1..
1

Batten Range: Wununmantyala sandstone/Masterton Sandstone: NW-SE Compression
60 42 S 5 W D 1 149 63 E 5 E D 13 141 80 W 8 E D 25
140 80 W 5 W D 2 146 70 E 23 E D 14 69 40 S 80 E R 26
133 49 S 10 E D 3 175 86 E 90 E R 15 74 61 S 75 E R 27
55 74 S 48 W D 4 139 64 W 10 E S 16 75 35 S 90 E R 28
170 89 E 20 W S 5 90 75 S 12 E D 17 135 73 E "11 W D 29
30 80 E 5 S S 6 175 80 W 80 E R 18 141 34 E 5 W D 30
125 67 S 12 W D 7 161 78 W 30 W D 19 146 43 E 0 E D 31
79 72 N 25 E D 8 75 27 E 90 E R 20 140 71 E 40 E D 32
79 69 N 45 W D 9 121 80 N 12 E D 21 135 69 E 16 E D 33
117 75 S 15 E D 10 123 70 S 30 W D 22 150 70 W 32 W D 34
72 46 E 90 E R 11 71 68 S 90 E R 23 153 61 E 11 E D 35
79 80 E 90 E R 12 141 82 W 10 W D 24 144 80 E 65 E N 36
MINIMISATION PERCENT 88 SELECTED PARAMETERS, SIGMA 1 TRE=167 PLUN=19
LEAST SQUARE REGRESSION OF THE 31CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 21. 94 ERROR IN R .45E+OO
NO STRESS vALUES USED AND PRINCIPAL AXES STRESS RATIO R = .37
SIGMA(l)= .54270 TREND 167.4 (ERR 4.6) PLUNGE 18.7 (ERR 4.51
SIGMA(2)= -.08541 TREND 337.8 (ERR 45.21 PLUNGE 71. 0 (ERR 4.91
SIGMA(3)= -.45730 TREND 76.4 (ERR 7.5) PLUNGE 3.0 (ERR 13.5)
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 7 9 25 28 5 33 14 21
2 .1 .2 14 20 8 10 12 11 6 19
3 .2 .3 17 23 2 34
4 .3 .4 21 30 32 27 24
5 .4 .5 27 3 26 31 35 13 7
6 .5 .6 28 29
7 .6 .7 28
8 .7 .8 30 17 36
9 .8 .9 31 22
10 .9 1.0 31
11 1.0 1.2 31
12 1.2 1.4 31
13 1.4 1.6 31
14 1.6 1.8 32 15
15 1.8 2.0 32
16 2.0 2.2 33 18
17 2.2 2.4 34 1
18 2.4 2.6 34.
19 2.6 2.8 34
20 2.8 3.0 35 16
21 3.0 3.2 36 4
SCHMIDT NET OF NEAREST EXACT SOLN
33
33 3 *2
33
3 3
­
3
3 3
3 3
... 2
2 .22 2 3 -3
2
222
2
22
2
3 ..
3
2
1
1
+ 11 1 1 1
+++11
1 111 1+
1
3
3.

Ba t ten Range: Wununmantyala Sandstone/Masterton Sandstone: NE-SW Compression
60 42 S 5 W D 1 153 73 E 10 W D 49
130 12 S 90 E R 2 121 80 N 12 E D 50
175 80 E 10 w D 3 123 70 S 30 w D 51
140 80 w 5 w D 4 71 68 S 90 E R 52
60 80 N 0 E S 5 61 62 S 14 w S 53
48 57 S 48 w D 6 133 69 S 19 N s 54
110 33 S 90 E R 7 159 75 E 0 E D 55
133 49 S 10 E D 8 135 89 E 0 E S 56
55 74 S 48 w D 9 153 73 w 0 E D 57
170 89 E 20 w S 10 125 79 S 0 E S 58
169 80 E 0 E D 11 141 82 W 10 W D 59
79 87 N 12 E S 12 141 80 W 8 E D 60
30 80 E 5 S S 13 69 40 S 80 E R 61
125 67 S 12 w D 14 127 79 S 12 w S 62
79 72 N 25 E D 15 74 61 S 75 E R 63
171 82 E 10 W D 16 175 26 E 40 W D 64
107 66 N 0 E S 17 145 14 E 90 E R 65
33 20 E 0 E D 18 144 28 E 90 E R 66
127 72 S 64 W R 19 133 31 N 90 E R 67
79 69 N 45 w D 20 151 63 E 70 E R 68
117 75 S 15 E D 21 47 71 S 31 W D 69
155 52 E 90 E R 22 175 84 E 11 W D 70
72 46 E 90 E R 23 144 40 E 90 E R 71
79 80 E 90 E R 24 158 67 E 20 w D 72
166 78 E 40 N D 25 129 71 N 7 E S 73
149 63 E 5 E D 26 166 38 E 12 w D 74
146 70 E 23 E D 27 161 41 E 57 w D 75
175 86 E 90 E R 28 174 78 E 10 W D 76
167 79 W 9 E D 29 140 52 w 60 w R 77
95 70 S 10 W S 30 157 63 E 17 w D 78
155 66 E 60 w R 31 151 12 E 69 w R 79
70 80 N 16 w S 32 79 64 N 0 E S 80
139 64 w 10 E S 33 153 78 E 5 E D 81
0 69 E 31 N D 34 75 35 S 90 E R 82
165 77 E 12 w D 35 164 81 E 0 E D 83
172 80 E 10 W D 36 135 73 E 11 W D 84
168 75 E 15 w D 37 141 34 E 5 W D 85
157 85 E 7 w D 38 146 43 E 0 E D 86
164 73 E 13 w D 39 140 71 E 40 E D 87
90 75 S 12 E D 40 135 69 E 16 E D 88
40 74 E 6 w D 41 148 58 E 90 E R 89
175 80 w 80 E R 42 157 42 E 90 E R 90
171 54 w 60 E R 43 150 70 w 32 w D 91
41 72 E 8 w D 44 171 75 w 20 w D 92
161 78 W 30 w D 45 161 80 w 5 E D 93
156 82 w 0 E D 46 172 64 E 15 w D 94
153 69 E 22 w D 47 153 61 E 11 E D 95
75 27 E 90 E R 48 144 80 E 65 E N 96
MINIMISATION PERCENT 62 SELECTED PARAMETERS, SIGMA 1 TRE=230 PLUN= 2 LEAST
SQUARE REGRESSION OF THE 59cLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 22.66202 ERROR IN R .48E+00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA{l}= .60708 TREND 230.9 (ERR 13.2) PLUNGE 2.0 (ERR 12.8)
SIGMA(2)= -.21417 TREND 86.1 (ERR 83.71 PLUNGE 87.5 (ERR 31.5)
SIGMA(3)= -.39292 TREND 321. 0 (ERR 13.1) PLUNGE 1.4 (ERR 51.2)
STRESS RATIO R = .18
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 14 36 75 76 80 38 3 16 37 64 69 30 66 71 6
2 .1 .2 27 41 65 35 44 70 79 56 31 18 67 11 29 32
3 .2 .3 36 94 39 83 5 12 19 34 2 89
4 .3 .4 39 93 43 17
5 .4 .5 46 72 25 62 90 46 77 22
6 .5 .6 51 55 47 78 58 49
7 .6 .7 54 53 81 74
8 .7 .8 57 92 73 7
9 .8 .9 60 54 68 57
10 .9 1.0 60
11 1.0 1.2 62 45 42
12 1.2 1.4 64 95 26
13 1.4 1.6 69 86 60 85 24 28
14 1.6 1.8 80 52 27 82 8 91 33 48 23 9 59 4
15 1.8 2.0 83 84 63 61
16 2.0 2.2 83
17 2.2 2.4 89 88 96 1 87 20 21
18 2.4 2.6 90 14
19 2.6 2.8 93 15 10 40
20 2.8 3.0 94 51
21 3.0 3.2 96 50 13

SCHMIDT NET OF NEAREST EXACT SOLN
.. -333 333
.. 33333 33 1 1 1
3 3 3 1.
3 3
3 11
1 .1
3 2
1..
3 2
2 2
2 22
22.22
2 22 2* ..
2 222. 2
2
2 2 23 2
2 2
11
.1 1
.1
.1+ 3 3
+++11
+1 1 1 3 3 33.
1. 1 1 3 33 33 .
.. 1 1 3 333.
333.
3 ...

Appendix 2b
Scrutton Range: Basal Tawal1ah Group: NE-SW Compression (1)
122 64 w 90 E R 1 51 71 E 5 E S 8
9 36 w 0 E D 2 145 50 E 0 E S 9
161 64 W 0 E D 3 130 68 E 7 W S 10
i75 75 E 0 E D 4 142 60 w 0 E S 11
137 64 W 0 E D 5 122 30 w 60 E S 12
72 71 E 5 E D 6 59 41 E 50 E S 13
11 61 W 0 E S 7
MINIMISATION PERCENT 60 SELECTED PARAMETERS, SIGMA 1 TRE=240 PLUN=10 LEAST
SQUARE REGRESSION OF THE 7 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 18.72711 ERROR IN R .13E+OO
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(l)= .34148 TREND 70.8 (ERR 30.4) PLUNGE 26.5 (ERR 87.2)
SIGMA(2)= .31703 TREND 267.2 (ERR 61.0) PLUNGE 62.6 (ERR 87.1)
SIGMA(3)= -.65852 TREND 164.2 (ERR 18.7) PLUNGE 6.7 (ERR 17.7)
STRESS RATIO R = .98
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 4 3 10 4 9
2 .1 .2 4
3 .2 .3 6 2 11
4 .3 .4 7 12
5 .4 .5 7
6 .5 .6 7
7 .6 .7 7
8 .7 .8 7
9 .8 .9 7
10 .9 1.0 7
11 1.0 1.2 8 13
12 1.2 1.4 8
13 1.4 1.6 9 6
14 1.6 1.8 9
15 1.8 2.0 9
16 2.0 2.2 10 1
17 2.2 2.4 11 8
18 2.4 2.6 11
19 2.6 2.8 11
20 2.8 3.0 12 5
21 3.0 3.2 13 7
SCHMIDT NET OF NEAREST EXACT SOLN
3
..... .
2
2
.......
•
3
-3
1+
+++
+
1

Scrutton Range: Basal Tawallah Group: NE-SW Compression (21
133 42 W 70 W R 1 145 38 W 70 W R 19 161 64 W 0 E D 37
122 64 W 90 E R 2 145 25 W 90 E R 20 175 75 E 0 E D 38
165 64 W 90 E R 3 172 37 W 70 E R 21 137 64 W 0 E D 39
164 46 W 90 E R 4 160 37 W 80 E R 22 72 71 E 5 E D 40
161 37 W 70 W R 5 173 27 W 80 E R 23 4 13 W 45 S D 41
158 32 W 70 E R 6 11 29 W 90 E R 24 164 89 W 0 E D 42
152 52 W 90 E R 7 14 44 W 75 S R 25 11 61 W 0 E S 43
170 21 W 80 E R 8 171 57 W 80 E R 26 82 71 E 5 E S 44
135 42 W 70 W R 9 9 36 W 0 E D 27 73 65 E 10 W S 45
136 39 W 70 W R 10 40 64 E 0 E D 28 51 71 E 5 E s 46
135 34 W 80 W R 11 28 65 E 0 E D 29 145 50 E 0 E S 47
137 22 W 90 E R 12 56 81 E 0 E D 30 100 87 S 0 E S 48
173 56 W 80 W R 13 31 64 E 5 E D 31 130 68 E 7 W S 49
173 41 W 90 E R 14 21 67 W 7 N D 32 142 60 W 0 E S 50
156 15 w 80 W R 15 17 64 W 10 W D 33 86 64 S 10 W S 51
149 22 W 70 W R 16 171 83 W 0 E D 34 122 30 W 60 E S 52
149 48 W 90 E R 17 8 84 W 0 E D 35 59 41 E 50 E S 53
144 34 W 80 W R 18 65 89 E 5 W D 36 97 89 N 5 W S 54
65 47 E 15 W S 55
MINIMISATION PERCENT 78 SELECTED PARAMETERS, SIGMA 1 TRE= 65 PLUN=10 LEAST
SQUARE REGRESSION OF THE 42 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 17.04976 ERROR IN R .16E+00
NO STRESS VALUES USED AND PRINCIPAL AXES STRESS RATIO R = .00
SIGMA(1l= .66655 TREND 67.4 (ERR 14.51 PLUNGE 2.7 (ERR 10.9)
SIGMA(2l= -.33310 TREND 336.9 (ERR ?) PLUNGE 11.2 {ERR ?l
SIGMA(3l= -.33345 TREND 170.6 (ERR ?) PLUNGE 78.4 (ERR ?l
GAMME NBRE rNDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 8 55 48 21 8 19 51 30 35
2 .1 .2 21 18 22 44 36 23 10 15 54 7 4 45 9 16
3 .2 .3 30 1 17 20 42 33 28 26 31 34
4 .3 .4 37 11 41 3 6 14 29 12
5 .4 .5 39 5 32
6 .5 .6 40 25
7 .6 .7 42 24 13
8 .7 .8 43 38
9 .8 .9 44 49
10 .9 1.0 45 27
11 1.0 1.2 47 50 2
12 1.2 1.4 48 47
13 1.4 1.6 49 37
14 1.6 1.8 49
15 1.8 2.0 50 52
16 2.0 2.2 50
17 2.2 2.4 51 39
18 2.4 2.6 53 53 43
19 2.6 2.8 53
20 2.8 3.0 53
21 3.0 3.2 55 40 46
SCHMIDT NET OF NEAREST EXACT SOLN
2 .. 2 2 2
... 2 2. 2
2 ..• 2 2
.. 2 2 2
2
2
3 11.
2
2 11
11
3 1 1 1.+
1+++
1 +.
3 1.
2 3 11
1 3
3
3 1.
•
11 3
3­
.1
..
1 3
.. 3
3
.11 2
1. 1
1 1 3
1
1. 22
2
3 2 2 ..
2 2 2 2 ..
2 22 ..
22 . .
.... .. 2 2

Scrutton Range: Middle and Upper Tawa11ah Group: NW-SE Compression
111 51 E 80 N N 1 114 40 W 45 W D 15 151 61 E 0 E S 29
14 88 W 50 W N 2 139 40 W 40 E D 16 114 22 W 10 E S 30
14 35 W 50 N R 3 165 33 E 5 W D 17 39 45 W 5 E S 31
34 83 W 60 E R 4 44 87 E 10 E S 18 5 62 W 0 E S 32
144 35 W 90 E N 5 42 47 W 20 W S 19 135 55 W 0 E S 33
136 57 W 80 W N 6 13 53 W 5 W S 20 163 34 W 90 E N 34
144 34 W 80 W N 7 11 84 E 5 E S 21 151 50 W 75 W N 35
157 46 W 90 E N 8 20 86 E 0 E S 22 162 77 W 60 W N 36
149 19 W 80 W N 9 14 81 E 15 E S 23 133 41 W 10 W D 37
76 61 W 0 E D 10 40 89 E 5 W S 24 160 39 W 20 W D 38
123 43 W 10 W D 11 45 38 E 30 E S 25 28 55 E 5 W S 39
72 80 W 30 E D 12 25 69 E 5 E S 26 11 77 E 0 E S 40
78 61 W 5 W D 13 25 74 E 30 E S 27 0 64 E 10 S S 41
99 74 N 0 E D 14 150 55 E 7 E S 28 66 81 E 0 E S 42
MINIMISATION PERCENT 75 SELECTED PARAMETERS, SIGMA 1 TRE=160 PLUN=16 LEAST
SQUARE REGRESSION OF THE 31 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 20.89404 ERROR IN R .34E"00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(l)= .35306 TREND 161.5 (ERR 13.6) PLUNGE 12.8 (ERR 80.1)
SIGMA(2)= .29389 TREND .6 (ERR 155.1) PLUNGE 76.4 (ERR 75.7)
SIGMA(3)= -.64694 TREND 252.5 (ERR 9.0) PLUNGE 4.3 (ERR 22.1)
STRESS RATIO R = .94
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 11 12 19 24 35 9 34 22 14 13 21 1
2 .1 .2 16 8 26 23 7 15
3 .2 .3 21 10 42 40 25 18
4 .3 .4 23 5 27
5 .4 .5 25 39 31
6 .5 .6 28 36 6 11
7 .6 .7 29 2
8 .7 .8 31 20 37
9 .8 .9 32 32
10 .9 1.0 32
11 1.0 1.2 34 41 38
12 1.2 1.4 35 4
13 1.4 1.6 35
14 1.6 1.8 38 17 3 16
15 1.8 2.0 38
16 2.0 2.2 40 29 28
17 2.2 2.4 42 33 30
SCHMIDT NET OF NEAREST EXACT SOLN
1
2 2
.. . 1 ..
1 2
11 1
.......
1 2 3
2 .3
1 2
22
2 1.
1 1 3.
22 3
'2
2 2
3 3 2 2 1
.3 3 2 1
.3- 2
.---3
.-33 1
3 3 1
. .. . 1 ..
2
1
211
1 2
11 1.
+
+++
+
. . 1 ...

Scrutton Range: Middle and Upper Tawa11ah Group: NE-SW Compression
102 60 S 60 w R 1 26 89 w 0 E 0 55
31 61 w 70 w R 2 165 33 E 5 w 0 56
141 34 w 70 w R 3 64 64 w 50 W 0 57
144 8 w 70 E R 4 72 55 E 0 E 0 58
162 5 w 90 E R 5 44 87 E 10 E S 59
144 44 w 90 E R 6 42 47 w 20 W S 60
1 31 E 90 N R 7 13 53 w 5 w S 61
171 51 E 80 N N 8 79 74 E 5 w S 62
14 88 w 50 w N 9 109 89 E 0 E S 63
1 30 w 70 N R 10 11 84 E 5 E S 64
115 21 w 90 E R 11 20 86 E 0 E S 65
160 17 w 90 E R 12 14 81 E 15 E S 66
129 26 w 70 w R 13 40 89 E 5 w S 67
159 41 w 50 W R 14 45 38 E 30 E S 68
14 35 w 50 N R 15 25 69 E 5 E s 69
158 37 w 50 w R 16 122 20 w 5 w S 70
161 40 w 70 w R 17 25 74 E 30 E S 71
5 51 w 90 N R 18 150 55 E 7 E S 72
131 35 w 80 w R 19 151 61 E 0 E S 73
34 83 W 60 E R 20 114 22 w 10 E S 74
154 49 W 50 w R 21 161 67 w 50 w S 75
155 25 w 90 E R 22 39 45 w 5 E s 76
158 85 w 90 E R 23 5 62 w 0 E S 77
151 22 w 90 E R 24 135 55 w 0 E S 78
98 15 S 50 w R 25 151 50 w 85 w R 79
109 16 w 60 w R 26 147 37 w 80 w R 80
144 35 w 90 E N 27 156 61 w 90 E R 81
136 57 w 80 w N 28 151 47 w 90 E R 82
144 34 w 80 w N 29 166 60 w 60 w R 83
157 46 w 90 E N 30 163 34 w 90 E N 84
149 19 w 80 w N 31 149 37 w 80 E R 85
66 56 E 5 w 0 32 149 26 w 80 w R 86
66 55 E 5 E 0 33 156 31 w 80 E R 87
60 61 E 0 E 0 34 139 25 w 90 E R 88
56 86 w 0 E 0 35 157 22 w 90 E R 89
76 61 w 0 E 0 36 136 22 w 90 E R 90
123 43 w 10 w 0 37 119 29 w 90 E R 91
72 80 w 30 E 0 38 160 35 w 80 w R 92
67 15 E 50 E 0 39 1 43 w 90 E R 93
40 89 w 5 w 0 40 151 50 w 75 w N 94
42 89 E 5 E 0 41 162 77 w 60 w N 95
20 62 W 10 E 0 42 171 57 W 70 W R 96
78 61 w 5 W 0 43 146 40 w 80 w R 97
176 84 E 0 E 0 44 169 28 w 80 w R 98
74 44 E 5 w 0 45 133 41 w 10 W 0 99
99 74 N 0 E 0 46 160 39 w 20 w 0 100
6 82 W 0 E 0 47 29 76 E 10 W 0 101
42 67 E 0 E 0 48 40 61 E 15 E 0 102
45 78 E 30 w 0 49 28 55 E 5 w S 103
114 40 w 45 w D 50 11 77 E 0 E S 104
44 88 E 10 E 0 51 0 64 E 10 S S 105
51 86 E 5 w 0 52 66 81 E 0 E S 106
42 58 w 5 E 0 53
139 40 w 40 E 0 54
MINIMISATION PERCENT 57 SELECTED PARAMETERS, SIGMA 1 TRE=255 PLUN= 5 LEAST
SQUARE REGRESSION OF THE 60 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 22.33187 ERROR IN R .20E+00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(l)= .65053 TREND 253.9 (ERR 17.3) PLUNGE 4.8 (ERR 2.51
SIGMA(2)= -.30105 TREND 163.9 (ERR 17.0) PLUNGE .9 (ERR 30.2)
SIGMA(3)= -.34947 TREND 63.1 (ERR 30.9) PLUNGE 85.1 (ERR 4.3)
STRESS RATIO R = .05
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 11 102 40 52 25 12 33 3 86 63 44 92
2 .1 .2 21 89 35 34 55 80 22 41 97 48 5
3 .2 .3 32 79 24 81 32 62 13 51 58 98 82 17
4 .3 .4 37 26 101 87 7 93
5 .4 .5 45 6 45 19 88 85 21 90 18
6 .5 .6 55 23 47 96 53 57 49 16 83 75 14
7 .6 .7 60 1 10 4 2 39
8 .7 .8 63 91 11 70
9 .8 .9 64 42
10 .9 1.0 66 78 74
11 1.0 1.2 69 72 38 73
12 1.2 1.4 71 15 54
13 1.4 1.6 72 56
14 1.6 1.8 72
15 1.8 2.0 74 20 100
16 2.0 2.2 76 105 77
17 2.2 2.4 78 61 99
18 2.4 2.6 82 76 9 37 103
19 2.6 2.8 85 28 95 27
20 2.8 3.0 95 71 104 43 59 36 69 29 60 30 66
21 3.0 3.2 106 50 68 31 46 64 65 94 8 84 106 67

SCHMIDT NET OF NEAREST EXACT SOLN
•• 2
.2
.. . 22 .
.. • 2
2
.. 2 ....
5
. . 1 1. .
1.
.1 1
1 111
11 1 1
33
33 3
---33
3"'3­
3
1
1
.11 333
.. 1
+1 1
.+++111
.+11 1
. . 11
.. 1
1 1
1 1
11 1
2.
2.
22
2 2 ..
2 .222222
..... 2 22 2 2 .... 2 .
..•.. 2.22 .•.•..

Appendix 2c
Tawallah Range: Basal Tawal1ah Group: NW-SE Compression
72 80 E 80 E N 1 112 34 W 20 W S 12 151 38 E 0 E 0 23
5 25 W 90 N R 2 103 62 E 7 E 0 13 116 75 E 0 E 0 24
22 68 E 80 E N 3 127 89 E 0 E 0 14 128 57 w 0 E 0 25
156 48 W 55 W R 4 72 86 E 5 W 0 15 129 64 E 7 E 0 26
22 85 W 5 E S 5 88 47 E 20 W 0 16 137 73 E 0 E 0 27
36 72 E 0 E S 6 75 84 E 15 W 0 17 72 73 E 7 E 0 28
103 72 S 5 E S 7 101 67 W 5 W 0 18 130 72 E 0 E D 29
128 89 E 0 E S 8 78 82 W 10 W 0 19 129 81 E 0 E D 30
125 89 W 0 E S 9 84 68 W 5 W .D 20 135 82 S 5 E D 31
131 69 W 0 E S 10 125 77 E 0 E D 21 144 25 E 0 E 0 32
15 43 W 0 E S 11 94 37 E 0 E D 22
MINIMISATION PERCENT 45 SELECTED PARAMETERS, SIGMA 1 TRE=300 PLUN=15 LEAST
SQUARE REGRESSION OF THE 14CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 14.86136 ERROR IN R .19E+00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(l)= .39044 TREND 302.9 (ERR 8.8) PLUNGE 9.5 (ERR 23.2)
SIGMA(2)= .21912 TREND 127.5 (ERR 19.9) PLUNGE BO.5 (ERR 23.2)
SIGMA(3)= -.60956 TREND 33.0 (ERR B.9) PLUNGE .7 (ERR 1.9)
STRESS RATIO R = .83
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 5 20 28 15 19 9
2 .1 .2 8 5 22 11
3 .2 .3 10 17 18
4 .3 .4 13 8 16 13
5 .4 .5 14 31
6 .5 .6 14
7 .6 .7 14
8 .7 .8 14
9 .8 .9 14
10 .9 1.0 14
11 1.0 1.2 16 24 10
12 1.2 1.4 16
13 1.4 1.6 17 3
14 1.6 1.8 22 1 4 25 26 21
15 1.8 2.0 23 2
16 2.0 2.2 25 29 32
17 2.2 2.4 29 30 12 23 27
18 2.4 2.6 30 7
19 2.6 2.B 32 6 14
SCHMIDT NET OF NEAREST EXACT SOLN
1
.1 +
+++ 1 1
+ 1
.. 3
1
3 ..
. 3.
2
2 2
'2
2 2
2
---3
1
3
1.

Tawal1ah Range: Basal Tawa11ah Group: NE-SW Compression(l)
158 33 E 90 E R 1 105 82 W 7 W S 64
121 25 E 80 W R 2 45 78 W 0 E S 65
149 42 W 90 E R 3 95 86 N 5 E S 66
72 80 E 80 E N 4 61 84 W 30 E S 67
5 25 W 90 N R 5 66 69 W 20 E S 68
22 68 E 80 E N 6 48 89 E 5 E S 69
142 83 W 90 E R 7 43 72 E 5 W S 70
122 30 W 90 E R 8 44 66 E 0 E S 71
140 17 W 90 E R 9 74 76 W 0 E S 72
156 48 w 55 W R 10 50 71 E 10 E S 73
138 48 W 70 E R 11 112 34 W 20 W S 74
162 50 W 60 E R 12 0 89 W 0 N D 75
145 55 W 65 E R 13 73 62 E 7 E D 76
147 58 W 60 E R 14 127 89 E 0 E D 77
134 34 W 90 E R 15 42 86 E 5 W D 78
144 72 W 80 E R 16 58 47 E 20 W D 79
144 53 W 90 E R 17 45 84 E 15 W D 80
140 49 W 70 E R 18 71 67 W 5 W D 81
128 22 w 70 E R 19 7 75 E 0 S D 82
122 33 W 80 W R 20 48 82 w 10 W D 83
145 50 W 75 E R 21 54 68 W 5 W D 84
129 56 W 70 E R 22 125 77 E 0 E D 85
141 46 W 90 E R 23 64 37 E 0 E D 86
142 36 W 85 W R 24 20 59 W 10 W D 87
145 38 W 90 E R 25 151 38 E 0 E D 88
134 43 W 80 W R 26 116 75 E 0 E D 89
138 46 W 70 E R 27 148 74 E 5 W D 90
143 55 W 80 W R 28 128 57 W 0 E D 91
125 80 W 90 E R 29 14 76 E 5 W D 92
149 29 W 70 W R 30 129 64 E 7 E D 93
129 32 W 75 W R 31 145 74 E 5 W D 94
22 85 W 5 E S 32 151 67 E 10 W D 95
36 72 E 0 E S 33 22 77 E 0 E D 96
42 63 E 10 E S 34 153 74 E 5 W D 97
74 89 E 20 W S 35 137 73 E 0 E D 98
111 78 E 5 E S 36 146 87 E 0 E D 99
73 89 E 7 W S 37 142 84 E 5 W D 100
105 84 S 40 W S 38 144 83 E 5 E D 101
111 75 W 10 W S 39 139 80 E 5 E D 102
114 89 E 5 W S 40 14 58 E 7 S D 103
103 72 S 5 E S 41 33 72 E 10 W D 104
95 75 S 7 W S 42 42 73 E 7 E D 105
101 86 S 0 E S 43 174 70 E 25 W D 106
91 71 S 15 W S 44 31 41 W 5 E D 107
128 89 E 0 E S 45 14 89 E 10 W D 108
66 88 E 5 W S 46 175 76 E 7 W D 109
55 89 E 0 E S 47 18 74 E 5 W D 110
110 89 E 30 W S 48 19 65 E 5 W D 111
46 74 E 0 E S 49 146 82 E 15 E D 112
75 84 E 5 W S 50 166 77 E 5 W D 113
121 89 W 50 W S 51 175 68 E 0 E D 114
125 89 W 0 E S 52 130 72 E 0 E D 115
48 68 E 5 W S 53 129 81 E 0 E D 116
72 73 E 5 W S 54 105 82 S 5 E D 117
81 72 E 0 E S 55 150 80 E 0 E D 11B
80 63 E 15 W S 56 144 25 E 0 E D 119
73 62 E 7 W S 57 165 89 E 5 E D 120
131 69 W 0 E S 58 153 76 E 0 E D 121
78 45 E 5 W S 59 7 73 E 0 E D 122
74 78 E 15 W S 60 23 77 E 5 E D 123
42 64 E 7 E S 61 8 73 E 5 S D 124
87 76 S 7 E S 62 22 73 E 0 E D 125
15 43 W 0 E S 63 23 75 W 45 W D 126
MINIMISATION PERCENT 75 SELECTED PARAMETERS, SIGMA 1 TRE=215 PLUN= 5 LEAST
SQUARE REGRESSION OF THE 94 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 16.99675 ERROR IN R .75E-01
NO STRESS VALUES USED AND PRINCIPAL AXES STRESS RATIO R = .,00
SIGMA(l)= .66605 TREND 218.6 (ERR 8.41 PLUNGE 6.3 (ERR ?)
SIGMA(2)= -.33210 TREND 356.9 (ERR ?) PLUNGE 81.6 (ERR ?)
SIGMA(3)= -.33395 TREND 128.0 (ERR ?) PLUNGE 5.6 (ERR ?)
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 26 107 60 13 37 70 125 113 82 14 72 109 20 96 46 122 34 108
61 53 120 110 92 18 65 87 104
2 .1 .2 44 51 15 101 47 71 21 50 100 8 111 11 49 124 123 27 118 75
66
3 .2 .3 67 99 69 36 9 12 35 114 29 54 38 56 48 106 97 103 121 40
31 44 23 68 57 26
4 .3 .4 77 2 25 22 112 73 90 24 43 19 17
5 .4 .5 85 55 42 16 64 102 95 94 3
6 .5 .6 89 59 62 28 67
7 .6 .7 92 126 1 39
8 .7 .8 94 30 7
9 .8 .9 97 41 98 74
10 .9 1.0 98 5
11 1.0 1.2 100 88 52
12 1.2 1.4 102 10 119
13 1.4 1.6 106 116 115 45 91
14 1.6 1.8 110 4 58 93 6
15 1.8 2.0 111 77
16 2.0 2.2 112 85
17 2.2 2.4 112
18 2.4 2.6 114 117 89
19 2.6 2.8 117 76 86 63
20 2.8 3.0 121 32 105 81 80
21 3.0 3.2 126 33 83 84 79 78

SCHMIDT NET OF NEAREST EXACT SOLN
.2.....
2 .. 1
2 1 1.
11.
2 1
.3 1 1
.. 333 1..
33 2
333 2
.. 2 2 33 2 1.
33
333 2
3 2 2
33 3 2
3 2 2.22 2
322 ... 2 2 2
2 2.22 2
2 22 2*22
222 33
2
2 2 33 22
.. 2 332
2 2 32 2
2 1 3 3
2 33
2 33
1 1 33
11 2 33 ­
11 1 2 ---.2
11 -3.
11+ 1 2
.. +++1111 2 2
11+11
.. 112 2 2
11
1
Tawal1ah Range: Basal Tawal1ah Group: NE-SW Compression(2)
72 80 E 80 E N 1 125 77 E 0 E D 10
5 25 W 90 N R 2 151 38 E 0 E D 11
22 68 E 80 E N 3 116 75 E 0 E D 12
156 48 W 55 W R 4 128 57 W 0 E D 13
36 72 E 0 E S 5 129 64 E 7 E D 14
103 72 S 5 E S 6 137 73 E 0 E D 15
131 69 W 0 E S 7 130 72 E 0 E D 16
112 34 W 20 W S 8 129 81 E 0 E D 17
127 89 E 0 E D 9 144 25 E 0 E D 18
MINIMISATION PERCENT 80 SELECTED PARAMETERS, SIGMA 1 TRE=200 PLUN= 5
LEAST SQUARE REGRESSION OF THE 14CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 14.52969 ERROR IN R .15E+00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(1)= .36538 TREND 192.9 (ERR 20.11 PLUNGE 29.5 (ERR 46.21
SIGMA(2)= .26924 TREND 44.4 (ERR 34.4) PLUNGE 56.5 (ERR 47.0)
SIGMA(J) = -.63462 TREND 291.4 (ERR 5.6) PLUNGE 14.6 (ERR 11.2)
STRESS RATIO R = .90
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 7 13 12 15 16 10 9 17
2 .1 .2 11 3 5 a 14
3 .2 .3 11
4 .3 .4 13 18 11
5 .4 .5 13
6 .5 .6 14 6
7 .6 .7 14
8 .7 .8 14
9 .8 .9 14
10 .9 1.0 14
11 1.0 1.2 14
12 1.2 1.4 14
13 1.4 1.6 14
14 1.6 1.8 15 1
15 1.8 2.0 15
16 2.0 2.2 15
17 2.2 2.4 15
18 2.4 2.6 15
19 2.6 2.8 15
20 2.8 3.0 17 4 7
21 3.0 3.2 18 2

E
E
z E
zz
+
+++
"[+
•

Tawallah Range: Wununmantyala Sandstone/Masterton Sandstone: NW-SE Compression
61 84 E 80 W N 1 91 71 E 3 E D 19 12 84 W 5 W S 37
158 75 E 80 E R 2 84 81 E 10 W D 20 130 80 W 10 E S 38
39 60 E 80 E R 3 75 85 E 7 E D 21 127 75 W 5 E S 39
90 72 S 55 E R 4 3 10 W 0 N D 22 135 22 W 10 W S 40
43 69 E 70 W R 5 77 67 E 7 E D 23 95 72 S 5 E S 41
50 53 E 80 E N 6 82 79 W 7 W D 24 178 74 E 0 E S 42
43 55 W 50 E N 7 85 55 W 20 W D 25 15 65 W 65 W R 43
40 61 E 70 E R 8 124 66 E 5 E D 26 104 67 E 5 E D 44
25 78 E 89 E N 9 80 77 E 5 E D 27 115 35 W 0 E D 45
176 77 E 89 N N 10 90 81 N 10 E D 28 75 89 E 5 W D 46
20 65 E 45 E N 11 134 77 E 5 W S 29 69 80 W 0 E D 47
146 80 E 60 W R 12 152 74 W 5 W S 30 65 76 E 5 W D 48
165 89 E 89 E N 13 145 76 W 17 E S 31 116 43 S 5 W D 49
175 18 E 89 E R 14 0 67 E 45 N S 32 81 62 W 0 E D 50
58 87 W 15 E D 15 5 83 W 3 S S 33 15 79 E 50 E D 51
114 75 W 45 W D 16 178 89 w 0 E S 34 133 71 W 0 E S 52
86 89 W 5 W D 17 177 89 E 10 N S 35 4 74 E 0 E S 53
80 86 W 11 W D 18 144 89 W 7 E S 36 167 89 E 10 E S 54
19 89 W 10 W S 55
MINIMISATION PERCENT 67 SELECTED PARAMETERS, SIGMA 1 TRE=120 PLUN= 8
LEAST SQUARE REGRESSION OF THE 36 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 19.56421 ERROR IN R .42E+00
NO STRESS VALUES USED AND PRINCIPAL AXES STRESS RATIO R = .37
SIGMA(1)= .54223 TREND 123.2 (ERR 12.1) PLUNGE 1.0 (ERR 2.5)
SIGMA(2)= -.08445 TREND 14.2 (ERR 9.9) PLUNGE 78.2 (ERR 31. 2)
SIGMA(3)= -.45777 TREND 219.4 (ERR 12.6) PLUNGE 11.7 (ERR 31.2)
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 11 17 19 36 55 21 54 27 18 24 34 46
2 .1 .2 17 30 38 31 29 44 40
3 .2 .3 20 20 33 23
4 .3 .4 27 49 35 47 28 52 39 50
5 .4 .5 31 37 42 25 15
6 .5 .6 34 8 48 43
7 .6 .7 36 53 3
8 .7 .8 36
9 .8 .9 36
10 .9 1.0 36
11 1.0 1.2 38 14 2
12 1.2 1.4 43 51 16 1 4 32
13 1.4 1.6 46 22 7 5
14 1.6 1.8 47 13
15 1.8 2.0 50 10 12 45
16 2.0 2.2 50
17 2.2 2.4 52 6 11
18 2.4 2.6 53 41
19 2.6 2.8 54 9
20 2.8 3.0 55 26
SCHMIDT NET OF NEAREST EXACT SOLN
. 111
.. 11
111
1
1 1
1 1
2
2
2 .2
2...22 2
2 2.22
222
'22
2
11
11+
3 1+++
3 1 .+
33 1 ..
.. 3 33- 3 3
.33 --- 3 3
.. 3-3 3
3
... 3
3
3
1
1

Tawa11ah Range: wununmantya1a Sandstone/Masterton Sandstone: NE-SW Compression
61 84 E 80 W N 1 24 84 W 45 W S 62
136 41 W 89 E R 2 5 83 W 3 S S 63
158 75 E 80 E R 3 178 89 W 0 E S 64
116 56 E 80 E R 4 177 89 E 10 N S 65
39 60 E 80 E R 5 51 73 E 5 E S 66
118 74 W 65 E R 6 49 64 E 10 W S 67
90 72 S 55 E R 7 144 89 W 7 E S 68
43 69 E 70 W R 8 44 73 E 5 E S 69
50 53 E 80 E N 9 81 74 W 5 E S 70
43 55 W 50 E N 10 64 87 W 3 E S 71
40 61 E 70 E R 11 12 84 W 5 W S 72
25 78 E 89 E N 12 31 84 W 0 E S 73
176 77 E 89 N N 13 130 80 W 10 E S 74
20 65 E 45 E N 14 27 86 E 5 W S 75
136 27 W 89 E R 15 80 89 E 0 E S 76
146 80 E 60 W R 16 80 89 E 0 E S 77
154 23 E 89 E R 17 40 90 W 7 W S 78
120 21 E 89 E R 18 62 83 E 5 E S 79
135 22 W 65 E R 19 42 70 W 0 E S 80
124 25 W 89 E R 20 127 75 W 5 E S 81
136 52 E 80 W R 21 65 81 E 22 W S 82
165 89 E 89 E N 22 66 85 W 5 W s 83
131 44 W 89 E R 23 52 76 E 10 E S 84
175 18 E 89 E R 24 55 68 E 5 E s 85
20 77 W 15 W D 25 27 68 E 11 W S 86
28 87 W 15 E D 26 55 65 W 0 E S 87
114 75 W 45 W D 27 135 22 W 10 W s 88
56 89 W 5 W D 28 95 72 S 5 E S 89
50 86 W 11 W D 29 30 78 E 10 W S 90
170 88 W 0 E D 30 60 89 W 10 W S 91
61 71 E 3 E D 31 178 74 E 0 E S 92
164 89 E 10 E D 32 81 82 E 5 W S 93
54 81 E 10 W D 33 45 26 E 5 E s 94
150 76 E 0 E D 34 15 65 W 65 W R 95
177 76 E 5 S D 35 74 67 E 5 E D 96
167 81 W 5 E D 36 14 89 E 0 E D 97
152 79 E 0 E D 37 6 89 E 10 N D 98
35 85 E 7 E D 38 15 64 E 5 E D 99
3 10 W 0 N D 39 115 35 W 0 E D 100
149 89 W 8 W D 40 35 89 E 5 W D 101
145 89 W 0 E D 41 27 61 E 30 E D 102
47 67 E 7 E D 42 39 80 W 0 E D 103
141 68 W 0 E D 43 35 76 E 5 W D 104
52 79 W 7 W D 44 131 82 W 0 E D 105
35 55 W 20 W D 45 173 64 W 5 E D 106
160 89 E 15 E D 46 86 43 S 5 W D 107
i24 66 E 5 E D 47 51 62 W 0 E D 108
50 77 E 5 E D 48 21 64 E 5 E D 109
133 74 E 5 E D 49 15 79 E 50 E D 110
60 81 W 10 E D 50 171 87 W 0 E D 111
165 67 W 7 E D 51 25 67 E 10 E D 112
132 76 E 0 E D 52 42 85 W 5 W S 113
127 81 E 0 E D 53 27 64 E 45 W S 114
95 78 S 10 W S 54 28 76 W 0 E S 115
134 77 E 5 W S 55 133 71 W 0 E S 116
30 89 W 5 W S 56 45 57 W 5 E S 117
49 64 E 19 E S 57 51 73 W 7 E S 118
152 74 W 5 W S 58 68 71 E 0 E S 119
145 76 W 17 E S 59 4 74 E 0 E S 120
38 49 E 7 E S 60 167 89 E 10 E S 121
0 67 E 45 N S 61 19 89 W 10 W S 122
MINIMISATION PERCENT 55 SELECTED PARAMETERS, SIGMA 1 TRE=200 PLUN= B LEAST
SQUARE REGRESSION OF THE 67 CLOSEST STRIATIONS
AVERAGE ERROR IN DEGREES 17.56022 ERROR IN R .12E+00
NO STRESS VALUES USED AND PRINCIPAL AXES
SIGMA(l)= .66192 TREND 204.2 (ERR 2.9) PLUNGE 5.1 (ERR 4.6)
SIGMA(2)= -.32384 TREND 105.6 (ERR 23.4) PLUNGE 59.0 (ERR 50.0)
SIGMA(3)= -.33808 TREND 297.2 (ERR 7.1) PLUNGE 30.5 (ERR 50.2)
STRESS RATIO R = .01
GAMME NBRE INDICE DES VALEURS DANS CETTE GAMME
1 .0 .1 15 113 80 78 90 102 117 83 97 56 .91 19 86 32 118 99
2 .1 .2 38 37 67 30 35 36 111 109 73 82 71 62 75 87 18 20 115 70
46 112 34 76 77 41
3 .2 .3 48 98 106 4 6 51 93 53 69 25 79
4 .3 .4 55 40 60 66 23 94 15 85
5 .4 .5 61 84 119 2 52 114 21
6 .5 .6 63 54 49
7 .6 .7 65 57 105
8 .7 .8 67 43 17
9 .8 .9 67
10 .9 1.0 70 110 16 89
11 1.0 1.2 74 8 95 24 47
12 1.2 1.4 74
13 1.4 1.6 79 7 22 5 100 3
14 1.6 1.8 83 13 11 9 88
15 1.8 2.0 84 1
16 2.0 2.2 84
17 2.2 2.4 91 81 12 116 107 14 10 27
18 2.4 2.6 94 61 96 74
19 2.6 2.8 99 58 26 31 42 45
20 2.8 3.0 107 48 55 38 65 59 39 50 122
21 3.0 3.2 122 108 29 44 64 121 68 103 104 63 92 101 33 120 28 72

SCHMIDT NET OF NEAREST EXACT SOLN
2
1 1 Ill.
1 1...
1 11..
2 11 1 ..
1 1
2 1..
2 1
•. 333
3 33
3--- 2
-333 2
3 2
2 333
333
2
3 22
2 2 22 22*2 22 2 2 2
2 22
2 3
33 22
2
2 3 3 2
23
2 2 2 3
22 3 3
2 2 3333.
1 2
.. 11
111 +111 1
.. 1 +++1
.. +111
2.

Appendix 3
3a Fluid inclusion microthermometry data
3b Fluid inclusion decrepitate microprobe analyses

Sample No. Fault type 8reccia type Incl. pop. UV ratio Te Tm-H20 Th NaCI eq.wt"1o Enthaply Chloride
93-802-2 Tawallah Fault Fracture 10 -6.2 227.2 9.5 17385 1.8
93-802-2 Tawallah Fault Fracture 5 -2.6 176.2 4.2 12883 0.75
93-802-2 Tawallah Fault Fracture 5 -41.2 -6.3 175.8 9.6 13211 1.82
93-802-2 Tawallah Fault Fracture 5 -8.2 338.8 11.9
93-802-2 Tawallah Fault Fracture 10 252.7
93-802-2 Tawallah Fault Fracture 10 -40.6 -2.1 226.4 3.4 17366 0.6
93-802-2 Tawallah Fault Fracture 5 -36.8 234.2
93-802-2 Tawallah Fault Fracture 5 -31.6 -7.6 144.2 11.2 10904 2.16
93-802-2 Tawallah Fault Fracture 5 -37.5 -7.6 190.1 11.2 14383 2.16
93-802-2 Tawallah Fault Fracture 5 -33.1 -7.6 151.7 11.2 11285 2.16
93-802-2 Tawallah Fault Fracture 10 253.2
93-802-2 Tawallah Fault Fracture 10 230.1
93-802-3 Tawallah Fault Fracture 10 343.8
93-802-3 Tawallah Fault Fracture 10 229.8
93-802-3 Tawallah Fault Fracture 1 5 168.3
93-802-3 Tawallah Fault Fracture 5 215.4
93-802-3 Tawallah Fault Fracture 10 -5.4 323.1 8.4
93-802-3 Tawallah Fault Fracture 10 -42.5 -5.3 321.1 8.2
93-802-3 Tawallah Fault Fracture 5 234.4
93-802-3 Tawallah Fault Fracture 5 195.4
93-802-3 Tawallah Fault Fracture 10 194.2 -
93-802-3 Tawallah Fault Fracture 5 -7.2 177.4 10.7 13411 2.05
93-802-3 Tawallah Fault Fracture 10 -33.7 -3.7 321.4 I 5.9 .....
93-802-3 Tawallah Fault Fracture 5 -38.6 -4.2 277.7 6.7 21642 1.23
93-802-3 TawaJlah Fault Fracture 5 179.3
93-802-3 Tawallah Fault Fracture 5 -4.3 239.2 6.8 21642 1.25
93-802-3 Tawallah Fault Fracture 5 232.6
93-802-4 Tawallah Fault Fracture 5 -38.2 -5.1 185.4 8 14025 1.49
93-802-4 Tawallah Fault Fracture 10 244.2
93-802-4 Tawallah Fault Fracture 5 -31.3 -5.6 _179.9 8.7 13632 1.63
93-802-4 Tawallah Fault Fracture 10 185.8
93-802-4 Tawallah Fault Fracture 5 180.2
93-802-4 Tawallah Fault Fracture 5 -22.6 187.8
93·802·4 Tawallah Fault Fracture 5 -25.2 -5 199.7 7.8 15216 1.45
93-B02-4 Tawallah Fault Fracture U 10 -42.6 -11.2 15.2
93-802-4 Tawallah Fault Fracture 5 -22.3 -9.6 157.3 13.5 11843 2.67
93-802-4 Tawallah Fault Fracture 30 -28.3 -5.1 243.6 8 18918 1.49
93-802-4 Tawallah Fault Fracture 50 -27.2 -5.3 249.2 8.2 19344 1.53
93-802-5 Tawallah Fault Fracture 5 -38 -7.3 226.7 10.9 16778 2.09
93-802-5 Tawallah Fault Fracture 5 -41.9 -5.2 232.4 8.1 17659 1.51
93-802-5 Tawallah Fault Fracture 5 -37.6 182.9
93-802-5 Tawallah Fault Fracture 5 -31.8 -2.8 176.6 4.5 13276 0.81
93-802-5 Tawallah Fault Fracture 5 -29.8 235.8
..._.­
93-802-5 Tawallah Fault Fracture 5 223.7
93-802-5 Tawallah Fault Fracture 5 250
93-803-1 Tawallah Fault Fracture 5 -42.3 -14.9 145.2 18.5 10779 3.88
93-803-1 Tawallah Fault Fracture 5 -47.3 -14.7 132.8 18.4 9856 3.86
93-803-1 Tawallah Fault Fracture 11 5 113
93-803-1 Tawallah Fault Fracture 11 20 -28.7
93-803-1 Tawallah Fault Fracture 11 5 -35.2 -2.7 138.6 4.4 10559 0.79
93-803-1 Tawallah Fault Fracture I1 30 -37.3 -9.6 127.6 13.5 9570 2.67
93-803-1 Tawallah Fault Fracture 1I 5 184.9
93-803-1 Tawallah Fault Fracture 11 5 -12.2 179.9 16.2 13477 3.31
93-803-1 Tawallah Fault Fracture 11 10 124.2
93-803-1 TawaJlah Fault Fracture 11 10 133.9
93-803-2 Tawallah Fault Fraclure n 5 -2.5 150.3 4.1 11329 0.73
93-803-2 Tawallah Fault Fracture 11 5 145
Appendix 3a Fluid inclusion microthermometry data (2)

Sample Ne. Fault type 8reccia typE Inc!. pop UV ratio Te Tm-H2C Th NaGI eq.wt° .Enthapl Chlorid
93-814-3 NW-sin Open 5 145.9
93-814-3 NW-sin Open 5 111.8
93-814-3 NW-sin Open 5 -36.4 -1.9 123.6 3.1 8861 0.55
93-814-3 NW-sin Open 5 -52.6 -1.3 2.1
93-815-1 NNW-dex Fracture 5 231.3
93-815-1 NNW-dex Fracture 10 -32.8 -9.2 109.3 13.1 8241 2.58
93-815-1 NNW-dex Fracture 5 172.3
93-815-1 NNW-dex Fracture 10 -38.9 -18.2 161.1 21.1 11847 4.58
93-815-1 NNW-dex Fracture 40 186.7
93-815-1 NNW-dex Fracture 30 -10.1 192.3 14.1 14542 2.81
93-815-1 NNW-dex Fracture 30 -37.3 -16.2 132.6 19.6 9829 4.17
93-815-1 NNW-dex Fracture 30 -42.5 -13.1 156.7 17 11576 3.5
93-815-1 NNW-dex Fracture 10 142.7
93-815-1 NNW-dex Fracture 10 202.6
93-815-2 NNW-dex Fracture 10 127.7
93-815-2 NNW-dex Fracture 10 -14.6 122.7 18.3 8109 3.83
93-815-2 NNW-dex Fracture [ 50 92.3
93-815-2 NNW-dex Fracture 11 5 -31 -14.5 167.2 18.2 12484 3.81
93-815-2 NNW-dex Fracture 11 20 -28.3 -15.2 137.1 18.8 10230 3.96
93-815-2 NNW-dex Fracture 20 -29.7 163.4 .•
93-815-2 NNW-dex Fracture 20 133.7
93-815-2 NNW-dex Fracture 20 125.6 - -­
93-815-2 NNW-dex Fracture 30 -36.9 -15.3 182.3 18.9 13621 3.99
93-815-2 NNW-dex
- 93-815-2 NNW-dex
93-815-2 NNV\I-dex
93-815-2 . NNW-dex
Fracture
Fracture
Fracture
Fracture
5
5
30
5
-36.2 -15.6 270.6
165.6
123.3
131.2
19.1 20518 4.04
-­
93-815-2 NNW-dex Fracture 10 -11.6 134.7 15.6 10100 3.16
93-815-3 NNW-dex Fracture 5 -30.2 -1.4 295.9 2.3 22518 4.39
93-815-3 NNW-dex Fracture 5 -28.1 -0.7 147.2 1.2 10922 3.6
93-815-3 NNW-dex Fracture 5 128.2
93-815-3 NNW-dex Fracture 5 186.5
93-815-3 NNW-dex Fracture 5 205.3
93-815-3 NNW-dex Fracture 5 167.4
93-815-3 NNW-dex Fracture 10 167.2 .­
93-815-3 NNW-dex Fracture 5 -25.6 -5.1 151.2 8 11305 1.49
93-815-3 NNW-dex Fracture 10 220.7
93-815-3 NNW-dex Fracture 5 231.4
93-816-1 NNW-dex Fracture 5 -39.6 129.6
93-816-1 NNW-dex Fracture 5 113.5
93-816-1 NNW-dex Fracture 5 166.8
"-_.'"­-­
93-816-1 NNW-dex Fracture 20 -48.6 -5.8 114.1 8.9 8640 1.67
93-816-1 NNW-dex Fracture 30 -38.1 -8.1 119.2 11.8 9000 2.29
93-816-1 NNW-dex Fracture 5 -35.6 -6.2 108.5 9.5 8053 1.8
93-816-2 NNW-dex Fracture 5 175.9
93-816-2 NNW-dex Fracture 5 177.1
93-816-2 NNW-dex Fracture 5 127.3
93-816-2 NNW-dex Fracture 10 154.9
93-816-2 NNW-dex Fracture 5 143.6
93-816-2 NNW-dex Fracture 60 -25.6 -12.3 114.5 16.2 8600 3.31
93-816-2 NNW-dex Fracture JI 30 117.6 -­
93-816-2 NNW-dex Fracture 11 10 101.8
93-816-2 NNW-dex Fracture 11 10 -31.6 -10.1 88.1 14.1
93-816-2 NNW-dex Fracture 11 20 -32.6 0 128.6 0 9641 0
93-816-2 NNW·dex Fracture 11 5 -20.7 -5.4 131.5 8.4 9778 1.57
93-816-2 NNW-dex Fracture 11 5 -24.9 -13.2 107.1 17.1 7925 3.53
93-816-2 NNW-dex Fracture 11 10 -28.6 -12.6 120.3 16.5 8946 3.38
Appendix 3a Fluid inclusion microthermometry data (7)

Appendix 4
Appendix 4a Structural geology of the study region
Appendix 4b Structural geology of the Batten Range
Appendix 4e Structural geology of the Scrutton Range
Appendix 4d Structural geology of the Tawallah Range - Region 1
Appendix 4e Structural geology of the Tawallah Range - Region 2
Appendix 4f Structural geology of the Tawallah Range - Region 3