西藏查藏错铜铅锌矿床成因：C-H-O-S-Pb同位素制约

姜军胜; 郑有业; 高顺宝; 徐净; 田坎; 黄亮亮; 张永超; 尹胜记

doi:10.3799/dqkx.2015.084

Volume 40 Issue 6

Jun. 2015

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Jiang Junsheng, Zheng Youye, Gao Shunbao, Xu Jing, Tian Kan, Huang Liangliang, Zhang Yongchao, Yun Sunggi, 2015. Genesis of Chazangcuo Cu-Pb-Zn Deposit, Tibet: Constraints from C-H-O-S-Pb Isotope Geochemistry. Earth Science, 40(6): 1006-1016. doi: 10.3799/dqkx.2015.084

Citation:

Jiang Junsheng, Zheng Youye, Gao Shunbao, Xu Jing, Tian Kan, Huang Liangliang, Zhang Yongchao, Yun Sunggi, 2015. Genesis of Chazangcuo Cu-Pb-Zn Deposit, Tibet: Constraints from C-H-O-S-Pb Isotope Geochemistry. Earth Science, 40(6): 1006-1016. doi: 10.3799/dqkx.2015.084

Citation:

Jiang Junsheng, Zheng Youye, Gao Shunbao, Xu Jing, Tian Kan, Huang Liangliang, Zhang Yongchao, Yun Sunggi, 2015. Genesis of Chazangcuo Cu-Pb-Zn Deposit, Tibet: Constraints from C-H-O-S-Pb Isotope Geochemistry. Earth Science, 40(6): 1006-1016. doi: 10.3799/dqkx.2015.084

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Genesis of Chazangcuo Cu-Pb-Zn Deposit, Tibet: Constraints from C-H-O-S-Pb Isotope Geochemistry

doi: 10.3799/dqkx.2015.084

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
3.
Faculty of Resource Exploration, Kimchaek University of Technology, Pyongyang 999093, DPR of Korea

Received Date: 2014-09-10
Publish Date: 2015-06-15

Abstract

Abstract

Chazangcuo Cu-Pb-Zn deposit, hosted by the Linzizong Group volcanic rocks in the west of Gangdese metallogenic belt, is a copper polymetallic deposit discovered in recent years. So far, the genesis of the deposit is still lack of clear understanding. The results of C, H, O, S, Pb isotopic analysis show that the δ¹³C_V-PDB values range from -5.60‰ to -2.40‰, δD_V-SMOW values range from -111.00‰ to -68.00‰, and δ¹⁸O_V-SMOW values range from -8.65‰ to 0.27‰, indicating that the ore-forming fluid mainly derived from the magma hydrothermal in the early time, however, with the mineralization continuing, the proportion of atmospheric precipitation gradually turned larger. δ³⁴S_CDT values range from 0.50‰ to 2.50‰ and possess the distribution characteristics of tower, indicating that the sulfur isotope derived from the single magma source. Lead isotope ratios are relatively stable and have large μ values (more than 9.58), possessing the characteristics of the upper crust lead. The lead isotope characteristics are similar to the ore sulfides from the deposits in the north subzone of Gangdese metallogenic belt, but obviously different from the lead isotope characteristics of volcanic rocks of Dianzhong Formation. Therefore, the authors infer that the source of ore-forming materials mainly came from the magmatic source of the upper crust. Combining with the geological characteristics of Chazangcuo deposit, and contrasting the typical magmatic hydrothermal vein-type deposit at home and abroad, the authors think that it belongs to the typical magmatic hydrothermal vein-type deposit.
- ore-forming fluid,
- ore-forming material,
- magmatic hydrothermal vein-type,
- ore deposit,
- tectonics

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References(72)

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Genesis of Chazangcuo Cu-Pb-Zn Deposit, Tibet: Constraints from C-H-O-S-Pb Isotope Geochemistry

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