冈底斯西段首例银锡多金属矿床的发现、成因及意义

高顺宝; 郑有业; 姜晓佳; 李伟良; 姜军胜

doi:10.3799/dqkx.2020.262

Volume 45 Issue 12

Dec. 2020

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Article Navigation > Earth Science > 2020 > 45(12): 4463-4480

Gao Shunbao, Zheng Youye, Jiang Xiaojia, Li Weiliang, Jiang Junsheng, 2020. Discovery, Genesis and Significances of First Siver-Tin Polymetal Deposit in Western Gangdese Belt. Earth Science, 45(12): 4463-4480. doi: 10.3799/dqkx.2020.262

Citation:

Gao Shunbao, Zheng Youye, Jiang Xiaojia, Li Weiliang, Jiang Junsheng, 2020. Discovery, Genesis and Significances of First Siver-Tin Polymetal Deposit in Western Gangdese Belt. Earth Science, 45(12): 4463-4480. doi: 10.3799/dqkx.2020.262

Citation:

Gao Shunbao, Zheng Youye, Jiang Xiaojia, Li Weiliang, Jiang Junsheng, 2020. Discovery, Genesis and Significances of First Siver-Tin Polymetal Deposit in Western Gangdese Belt. Earth Science, 45(12): 4463-4480. doi: 10.3799/dqkx.2020.262

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Discovery, Genesis and Significances of First Siver-Tin Polymetal Deposit in Western Gangdese Belt

doi: 10.3799/dqkx.2020.262

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Sino Shaanxi Nuclear Industry Group Geological Survey Co. Ltd., Xi'an 710100, China
4.
Wuhan Center of Geological Survey, CGS, Wuhan 430205, China

Received Date: 2020-07-08
Publish Date: 2020-12-15

Abstract

Abstract

The Balong Ag-Sn polymetallic deposit was newly discovered in the volcanic rock area of western Gangdese by mineral resources investigation project. The surface ore bodies are vein type ore bodies controlled by the coupling of thrust belt, volcanic mechanism and secondary faults in the margin of volcano-sediment graben basins. In order to find out the genesis of Balong deposit, the zircon U-Pb geochronology, ore mineralogy, mineral geochemistry and S-Pb isotopes were carried out. The results show that the weighted average age of zircon LA-ICP-MS U-Pb is 126.5±1.2 Ma in the ore-bearing volcanic rocks, the mineral assemblage is mainly composed of medium-low temperature minerals and a small amount of medium-high temperature minerals, the Zn/Cd and Zn/Fe ratios of sphalerite are 321-17 407 and 2.4-4.4, the Co/Ni ratio of pyrite is 2.2-3.6, the δ ³⁴S value of sulfide changes from 2.94 ‰ to 4.48 ‰, the ²⁰⁶Pb/²⁰⁴Pb ratio is 18.590-18.779, the ²⁰⁷Pb/²⁰⁴Pb ratio is 15.636-15.865, the ²⁰⁸Pb/²⁰⁴Pb ratio is 38.883-39.991.The above results show that the formation of the deposit is closely related to the subvolcanic hydrothermal fluid of the late stage of Early Cretaceous volcanic activity in the western Gangdese, and the ore-forming materials have the characteristics of magmatic sulfur and lead in the upper crust. Compared with the typical Ag-Sn polymetallic deposits in the world, the metallogenic characteristics of the Balong deposit are similar to those of the world's large-superlarge scale Ag-Sn polymetallic deposits. The surface ore body belongs to the epithermal silver-polymetallic orebody, and the porphyry tin-polymetallic orebody may develop downward. The metallogenic characteristics of Ag-rich and Sn-bearing deposit in the western Gangdese are firstly discovered. This discovery not only provides new data and constraints for the study of the genetic types of the deposits in the volcanic rock area of the western Gangdese, but also greatly broadens the prospecting horizon in the area.
- Ag-Sn polymetallic,
- continental volcanism,
- porphyry-epithermal type,
- western Gangdese belt,
- deposits

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致谢: 在成文过程中，3位匿名审稿专家对本文提出了大量建设性修改意见，使得论文质量得到明显提高，在此一并表示诚挚的谢意！同时，2020年是中国地质大学（武汉）地质调查研究院成立二十周年，二十年来中国地质大学（武汉）地质调查研究院为我国地调事业做出了突出贡献，谨以此文祝愿中国地质大学（武汉）地质调查研究院在新时代地调事业中再创辉煌！

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