四川乌斯河铅锌矿床成矿流体特征及TSR作用初探

熊索菲; 姚书振; 宫勇军; 谭满堂; 曾国平; 王伟

doi:10.3799/dqkx.2016.008

Volume 41 Issue 1

Jan. 2016

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Article Navigation > Earth Science > 2016 > 41(1): 105-120

Xiong Suofei, Yao Shuzhen, Gong Yongjun, Tan Mantang, Zeng Guoping, Wang Wei, 2016. Ore-Forming Fluid and Thermochemical Sulfate Reduction in the Wusihe Lead-Zinc Deposit, Sichuan Province, China. Earth Science, 41(1): 105-120. doi: 10.3799/dqkx.2016.008

Citation:

Xiong Suofei, Yao Shuzhen, Gong Yongjun, Tan Mantang, Zeng Guoping, Wang Wei, 2016. Ore-Forming Fluid and Thermochemical Sulfate Reduction in the Wusihe Lead-Zinc Deposit, Sichuan Province, China. Earth Science, 41(1): 105-120. doi: 10.3799/dqkx.2016.008

Citation:

Xiong Suofei, Yao Shuzhen, Gong Yongjun, Tan Mantang, Zeng Guoping, Wang Wei, 2016. Ore-Forming Fluid and Thermochemical Sulfate Reduction in the Wusihe Lead-Zinc Deposit, Sichuan Province, China. Earth Science, 41(1): 105-120. doi: 10.3799/dqkx.2016.008

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Ore-Forming Fluid and Thermochemical Sulfate Reduction in the Wusihe Lead-Zinc Deposit, Sichuan Province, China

doi: 10.3799/dqkx.2016.008

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Collaborative Innovation Center for Exploration of Strategic Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Wuhan Center, China Geological Survey, Wuhan 430200, China

Received Date: 2015-09-29
Publish Date: 2016-01-15

Abstract

Abstract

The Wusihe lead-zinc deposit, hosted in the Dengying Formation, is a large lead-zinc deposit in the Sichuan Province, China. The previous research noted the Wusihe deposit was classified as a sediment-hosted stratiform lead-zinc deposit. However, our field survey result suggests that hydrothermal ore-forming processes are crucial to lead-zinc mineralization. In this paper, we present a detailed petrographic, microthermometric and laser Raman spectroscopy study of fluid inclusions from the Wusihe deposit reveals the characteristics of ore-forming fluids and mineralization mechanism. Primary fluid inclusions (FIs) in dolomite, quartz, calcite, fluorite and sphalerite are mainly two phases (L+V type). Microthermometric data show the homogenization temperatures range from 120 ℃ to 260 ℃, and the average of salinity is 10.0% NaCl eqv. The estimated trapping pressures are 32 MPa to 68 MPa. The laser Raman spectroscopy shows that the gas components have a certain amount of CH₄, H₂S, C₂H₆, C₂H₂, N₂ and NH₃. The mixed ore-forming fluids offer heat, SO₄^2-, and Mg²⁺ to provoke the thermochemical sulfate reduction (TSR). The TSR could be a key factor for sulfur source and H⁺. The change of pH value leads to the precipitation of metallogenic elements.
- ore-forming fluid,
- fluid inclusions,
- lead-zinc deposit,
- thermochemical sulfate reduction,
- geochemistry.

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References(77)

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