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WU Yan-shuang, WANG Li-jin, ZHOU Ke-fa, LIU Yan-bin. Research on Fluid Inclusion Analysis of Jiamante Gold Deposit in Xinjiang[J]. Rock and Mineral Analysis, 2012, 31(3): 507-510.
Citation: WU Yan-shuang, WANG Li-jin, ZHOU Ke-fa, LIU Yan-bin. Research on Fluid Inclusion Analysis of Jiamante Gold Deposit in Xinjiang[J]. Rock and Mineral Analysis, 2012, 31(3): 507-510.
shu

Research on Fluid Inclusion Analysis of Jiamante Gold Deposit in Xinjiang

  • 1.

    College of Geology and Exploration Engineering, Xinjiang University, Urumqi 830047, China

  • 2.

    College of Geology and Exploration Engineering, Xinjiang University, Urumqi 830047, China

  • 3.

    Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Geography and Ecology, Chinese Academy of Sciences, Urumqi 830011, China

  • 4.

    College of Geology and Exploration Engineering, Xinjiang University, Urumqi 830047, China

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  • Received Date: October 21, 2011
  • Revised Date: March 08, 2012
    Abstract
  • The salinity and density of fluid inclusions in quartz, sphalerite and calcite hosted in gold-bearing veinlets of Jianante gold deposit, Xinjiang, were studied by micro temperature measurement measurement. Also, the components in fluid inclusions were studied by using Laser Raman Spectrometry. The results indicate that only a H2O peak was shown on the Laser Raman spectrum atlas for all fluid inclusions, which was attributed to the NaCl-H2O system. Homogeneous temperatures ranged from 180℃ to 260℃ with salinities in the range of 0.17%-12.52% and densities in the range of 0.49-0.97 g/cm3. This indicates that ore-forming fluids are characterized by low temperature, low salinity and low density. The conclusion is that the Jiamante Au deposit is an epithermal deposit.
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    • References (14)
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