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| Keywords | |
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West Kunlun |
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Kalayasikake |
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ore-controlling structure |
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metallogenic model |
| Authors | |
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YU Huan-Tao-1 |
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2 |
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LIU Ji-Shun-1 |
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2 |
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LIU Wen-Heng-1 |
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2 |
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WANG Tian-Guo-1 |
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2 |
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LI Xi-1 |
| PubMed | |
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Article by Yu, H. T. 1 |
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Article by 2 |
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Article by Liu, J. S. 1 |
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Article by 2 |
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Article by Liu, W. H. 1 |
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Article by 2 |
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Article by Wang, T. G. 1 |
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Article by 2 |
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Article by Li, X. 1 |
Ore-controlling structure and metallogenic model of Kalayasikake Pb-Zn-Cu polymetallic deposit in West Kunlun
YU Huan-Tao-1, 2, LIU Ji-Shun-1, 2, LIU Wen-Heng-1, 2, WANG Tian-Guo-1, 2, LI Xi-1
1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals��Ministry of Education��Central South University�� Changsha 410083��China; 2. School of Geosciences and Info-Physics��Central South University��Changsha 410083��China
The authors studied the ore-controlling structure and metallogenic model of Kalayasikake of West Kunlun using geological and geochemical methods�� ��esearch on deposit geochemistry found δ34 S as �� 5. 3‰ �� �� 32. 6‰��206Pb /204Pb as 17. 712 �� 18. 082��207Pb /204Pb was 15. 358 �� 15. 664 and 208Pb /204Pb as 37. 513 �� 38. 399 in contents�� The research showed that deep-metallogenic materials upwelled to surface along with the deep faults as to tectonic force or others during Devonian-Carboniferous��and deposited with detrital materials to form source beds�� After that��the hydrotherm formed by the extraction with atmospheric rainwater��and then transported and concentrated�� that was the formation of ore source bed�� The mild-overthrust fault ( transmitting ore structure) and the steep-thrust fault including the joint-fissure came from it ( ore-hosting structures) in the mining area controlled the formation of ore body��