西藏普兰县姜叶马豆荚状铬铁矿地质特征及找矿前景
西藏普兰县姜叶马豆荚状铬铁矿地质特征及找矿前景
西藏普兰县姜叶马豆荚状铬铁矿地质特征及找矿前景
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
2006 Geology and M ineral Resources of South China3<br />
: 1007 - 3701 (2006) 03 - 0055 - 06<br />
<br />
,,,<br />
(, 443003)<br />
:,<br />
<br />
<br />
<br />
,,<br />
,<br />
:;; ;;<br />
: P618. 33: A<br />
,,<br />
,,OPX,<br />
,15%<br />
<br />
:80 4680<br />
54 ,30 463073% ,<br />
50<br />
1<br />
(1) <br />
1. 1<br />
750 km 2 (1987,)<br />
,<br />
(N<br />
() :<br />
2 z)<br />
,( K - A r<br />
(1):4% ,<br />
)98. 3 Ma, <br />
<br />
1. 2<br />
<br />
<br />
(2): 13% ,<br />
, <br />
,,<br />
, <br />
,<br />
,,2070<br />
: 2006 - 05 - 30<br />
:<br />
(1212010530108).<br />
:( 1965) ,,,<br />
.<br />
(3):,<br />
,<br />
(4)- :<br />
10% ,<br />
,() ()<br />
,NE,50<br />
60NW NEE<br />
() ,<br />
,,
56<br />
2006 <br />
1<br />
Fig. 1Geological sketch map of the Laangcuo body, Pulan Country<br />
,1 2,<br />
,2 km5 km,<br />
,,,<br />
, NW , NEE(1) <br />
, 2. 2<br />
,<br />
2<br />
12,8, 7. 26% , 0. 0061% , 0. 0045% ; Cr 2 O 3 /FeO =<br />
32 ()8 3. 63<br />
km2 km,NE; Cr2,;<br />
<br />
,60 m15 m60% 80% ,SiO 2 , S, P<br />
(2) <br />
2. 1()<br />
(),<br />
(Cr 2 O 3 32% )<br />
,80% 90% ,<br />
95% ,40. 98%<br />
SiO 2 , S, P,<br />
5,( 10% Cr 2 O 3 < 32% ),<br />
, <br />
- - <br />
<br />
5()<br />
,,,<br />
<br />
,, Cr 2 <br />
<br />
( ZK601) 5. 877. 98 m ,<br />
,<br />
2. 11 m() - - - -
3<br />
:<br />
57<br />
2<br />
Fig. 2Geological sketch map of the J iangyema chrom ite m ine area, Pulan Country<br />
- (O s, Ir, Ru, Rh, Pt,<br />
Pd)167. 76364. 59 10 - 9 ,Cr1 ,<br />
5 526 10 - 9 ,,3001200 m;<br />
()<br />
3<br />
,500800 m;<br />
- ,,<br />
,<br />
<br />
3. 1 <br />
,<br />
,<br />
,- <br />
( 10% ),<br />
300700 m;- <br />
(1015% ),<br />
; ,<br />
,<br />
[ 1 ] :,<br />
, 100200 m;- <br />
[ 1 ] , ,400500 m;<br />
,,,200300m
58<br />
2006 <br />
1()<br />
Table 1Geolog ica l character istics of the ore bod ies in J iangyema chrom ite deposit<br />
(m) (m) Cr 2 O 3 (w B /10 - 2 )<br />
Cr1 - 1 10. 60 1. 00 60 /50 42. 72<br />
Cr1 - 2 4. 20 0. 50 310 44. 81<br />
Cr2 - 1 1. 65 1. 30 320 /50 ,28. 4240. 85<br />
Cr2 - 2 6. 90 5. 50 60 ,47. 7551. 51<br />
Cr2 - 3 7. 60 5. 10 345 ,38. 4051. 96<br />
Cr2 - 4 3. 10 0. 70 110 51. 1851. 65<br />
Cr2 - 5 3. 40 0. 080. 40 220 /68 49. 99<br />
Cr3 - 1 5. 20 1. 10 295 /90 45. 38<br />
Cr3 - 2 2. 20 0. 60 310 53. 44<br />
Cr4 2. 40 0. 50 305 / sw 45. 21<br />
Cr5 2. 30 0. 60 30 42. 24<br />
Cr6 8. 00 0. 60 75 36. 9741. 15<br />
Cr7 2. 00 0. 30 340 11. 60<br />
Cr8 4. 20 1. 60 165 ,17. 1639. 48<br />
Cr9 6. 00 0. 70 128 ,31. 0336. 19<br />
Cr10 5. 00 0. 20 30 50. 72<br />
Cr11 6. 00 1. 50 115 19. 21<br />
Cr12 4. 00 1. 50 170 /28 21. 80<br />
Cr13 5. 00 0. 09 92<br />
, 49. 02<br />
Cr14 - 1 1. 40 0. 90 240 , 42. 90<br />
Cr14 - 2 1. 20 0. 20 , 44. 24<br />
Cr15 2. 00 0. 60 10 49. 76<br />
Cr16 - 1 1. 00 0. 50 140 45. 85<br />
Cr16 - 2 0. 80 0. 30 <br />
Cr17 0. 60 0. 05 20 <br />
Cr18 1. 20 0. 20 SN 42. 12<br />
Cr19 0. 50 0. 08 110 39. 25<br />
Cr20 24m 2 , 51. 18<br />
Cr2 ( ZK601) 2. 11 ,18. 1137. 52<br />
:, 2004, 2005
3<br />
:<br />
59<br />
,,<br />
, <br />
3. 2 4. 1<br />
<br />
()<br />
, (Cr’60)(Cr’> 60)<br />
[ 1 ] :<br />
:( <br />
),<br />
;- : <br />
,,<br />
;,Mg[Mg<br />
=<br />
; 100Mg/ (Mg + Fe 2 +<br />
) ] Cr ’[ Cr=<br />
- ,- 100Cr/ (Cr + A l) ],FeO, A l 2 O 3 <br />
;,<br />
,<br />
(3) <br />
,Cr’<br />
3<br />
(, 1999,) [ 1 ]<br />
Fig. 3The sketch map showing the columnar section of the<br />
m inerogenic position among the Laangcuo, Luobusha<br />
and Dongqiao bodies<br />
1. ; 2. ; 3. ; 4. ; 5. <br />
; 6. ; 7. ; 8. <br />
; 9. - ; 10. ; 11. <br />
; 121<br />
4<br />
7080,;<br />
MgO (41. 98% ) <br />
( 42. 74% ) ( 44. 21% );<br />
A l 2 O 3 (1. 40% ) <br />
(1. 26% ) ( 0. 95% ); <br />
, <br />
<br />
4. 2<br />
<br />
:<br />
,,<br />
,;,<br />
<br />
,,,<br />
,<br />
(Cr11 Cr12,<br />
2) ,( Cr11 <br />
19. 21% Cr1221. 80% ) ,(<br />
) ,350,<br />
,,<br />
Cr11Cr12<br />
,,<br />
,12,<br />
,
60<br />
2006 <br />
,:<br />
[ 24 ] , [ 1 ],,,. [M ]. <br />
:, 1999. 145146, 297306.<br />
,<br />
[ 2 ]. <br />
,,<br />
[ J ]. , 1996, 9 (4) : 452.<br />
<br />
[ 3 ],,. <br />
,,<br />
[ J ]. , 1996, 1: 6364.<br />
,<br />
[ 4 ]. [ J ]. <br />
, , 1996, 1: 94105.<br />
,<br />
<br />
Prospect for the J iangyema Podiform Chrom ite Deposit and its<br />
Golog ica l Character istics in Pulan Country, Tibet<br />
LE I Yi2jun , HUANG Guei2cheng , X IDe2m ing , L IL i2juan<br />
( Yichang institute of Geology and M ineral Resources , Yichang , 443003 , Hubei , China )<br />
Abstract: J iangyema chrom ite deposit lies in the Laangcuo rock body of which locates in the western<br />
Yaluzangbujiang ultramafic rock belt. It is a sort of the Cr2rich podiform chrom ite deposit. This article mostly<br />
discuss p rospect for the J iangyema podiform chrom ite deposit and its gological characteristics in Pulan Country,<br />
Tibet. According to the analysis of the rockfacies characteristics of Laangcuo rock body, investigated podiform<br />
chrom ite belt and ore spots of which have been discovered in J iangyema chrom ite m ine area, compared with<br />
chrom ite deposits of Luobusha and Dongqiao in Tibet. In this paper summarized the rule of the ore bodies distri2<br />
bution and their occurrence. This area exists geological condition for form ing podiform deposits on large scale<br />
and rep resents good p rospecting potentiality.<br />
Key words: podiform chrom ite deposit ; geological characteristics ; rule of the ore bodies occurrence ;<br />
p rospecting potentiality ; J iangyema