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    Volume 43 Issue 6
    Jun.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(6): 2076-2099
    Wang Jian, Zhang Jun, Zhong Wenbin, Yang Qing, Li Fake, Zhu Zhengkun, 2018. Sources of Ore-Forming Fluids from Tianbaoshan and Huize Pb-Zn Deposits in Yunnan-Sichuan-Guizhou Region, Southwest China: Evidence from Fluid Inclusions and He-Ar Isotopes. Earth Science, 43(6): 2076-2099. doi: 10.3799/dqkx.2018.601
    Citation: Wang Jian, Zhang Jun, Zhong Wenbin, Yang Qing, Li Fake, Zhu Zhengkun, 2018. Sources of Ore-Forming Fluids from Tianbaoshan and Huize Pb-Zn Deposits in Yunnan-Sichuan-Guizhou Region, Southwest China: Evidence from Fluid Inclusions and He-Ar Isotopes. Earth Science, 43(6): 2076-2099. doi: 10.3799/dqkx.2018.601
    shu

    Sources of Ore-Forming Fluids from Tianbaoshan and Huize Pb-Zn Deposits in Yunnan-Sichuan-Guizhou Region, Southwest China: Evidence from Fluid Inclusions and He-Ar Isotopes

    doi: 10.3799/dqkx.2018.601
    • 1.

      Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

    • 2.

      Guangxi Branch, China National Geological Exploration Center of Building Material Industry, Guilin 541001, China

    • 3.

      Yunnan Metallurgical Resources, Ltd., Kunming 650000, China

    • Received Date: 2018-01-10
    • Publish Date: 2018-06-15
      Abstract
    • In order to constrain the source of the ore-forming fluids in large Pb-Zn deposits in the Sichuan-Yunnan-Guizhou region, fluid inclusions and He-Ar isotopes have been analyzed in ore-forming fluids trapped in sulphide minerals from the large Tianbaoshan Pb-Zn deposit and the super large Huize Pb-Zn deposit. The results are summarized as follows:(1) Fluid inclusions in Tianbaoshan deposit have medium-low homogenization temperatures and medium salinities, and ore-forming fluids are mainly derived from basin brine, whereas fluid inclusions in Huize deposit represent high-medium homogenization temperatures and medium salinities, and ore-forming fluids are dominantly derived from basin brine, but with evidence for mixing of different fluids. (2) The values of 3He/4He in Tianbaoshan deposit and Huize deposit range from 0.02 to 0.32 Ra (where Ra is the atmospheric value; 3He/4He=1.4×10-6), indicating that the ore-forming fluids are dominated by continental crust fluids, where as a small but clear mantle helium contribution is present. And the measurements of 40Ar/36Ar ratio (345.0-1 698.8) indicate that the ore-forming fluids mainly consist of saturated atmospheric water. (3) Combined with geological features, fluid inclusion trapped in sulphide minerals and He-Ar isotopes, it is concluded that the ore-forming processes of Tianbaoshan deposit and Huize deposit are related to the evolution of Youjiang sedimentary basin and the magmatic activities of the Emeishan large igneous province.

       

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