藏南马扎拉金-锑矿床:成矿流体性质和成矿物质来源

谢玉玲; 杨科君; 李应栩; 李光明; 曲云伟; 董磊

doi:10.3799/dqkx.2019.122

Volume 44 Issue 6

Jun. 2019

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Article Navigation > Earth Science > 2019 > 44(6): 1998-2016

Xie Yuling, Yang Kejun, Li Yingxu, Li Guangming, Qu Yunwei, Dong Lei, 2019. Mazhala Gold-Antimony Deposit in Southern Tibet: The Characteristics of OreForming Fluids and The Origin of Gold and Antimony. Earth Science, 44(6): 1998-2016. doi: 10.3799/dqkx.2019.122

Citation:

Xie Yuling, Yang Kejun, Li Yingxu, Li Guangming, Qu Yunwei, Dong Lei, 2019. Mazhala Gold-Antimony Deposit in Southern Tibet: The Characteristics of OreForming Fluids and The Origin of Gold and Antimony. Earth Science, 44(6): 1998-2016. doi: 10.3799/dqkx.2019.122

Citation:

Xie Yuling, Yang Kejun, Li Yingxu, Li Guangming, Qu Yunwei, Dong Lei, 2019. Mazhala Gold-Antimony Deposit in Southern Tibet: The Characteristics of OreForming Fluids and The Origin of Gold and Antimony. Earth Science, 44(6): 1998-2016. doi: 10.3799/dqkx.2019.122

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Mazhala Gold-Antimony Deposit in Southern Tibet: The Characteristics of OreForming Fluids and The Origin of Gold and Antimony

doi: 10.3799/dqkx.2019.122

1.
Civil and Resource Engineering School, University of Science and Technology Beijing, Beijing 100083, China
2.
Beijing Jinyou Exploration Limited Company, Beijing 100010, China
3.
Chengdu Center, China Geological Survey, Chengdu 610081, China

Received Date: 2019-04-16
Publish Date: 2019-06-15

Abstract

Abstract

The genesis of Mazhala Au-Sb deposit, which is one of the most important Au-Sb deposits in South Tibet Au-Sb metallogenic belt, is still open to debate. Based on field observation, petrography, microscopy, fluid inclusions, and stable isotopic results, in this paper, it discusses the characteristics of ore-forming fluid, the transportation, and the precipitation mechanism of Au and Sb. It can be concluded that the ore-formng fluid has a dominant magmatic origin, and is of moderate temperature (ca.255℃), low salinity (ca.2.8%-3.5% NaCleqv) and rich in CO₂. The estimated ore-forming pressure is about 150 MPa. The unmixing between CO₂ and aqueous during the fluid evolution leads to the ore precipitation. The Au, Sb may have been sourced from wall rocks, especially the submarine volcanic rock of them.
- South Tibet Au-Sb metallogenic belt,
- Mazhala Au-Sb deposit,
- fluid inclusion,
- source of Au and Sb,
- deposits

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References(89)

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Mazhala Gold-Antimony Deposit in Southern Tibet: The Characteristics of OreForming Fluids and The Origin of Gold and Antimony

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