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LI Junsheng, XU Dong, LANG Zhen, et al. The Fluid Inclusion Characteristics and Significance of the Huaishuping Gold Depositin Song County, Henan province[J]. Northwestern Geology, 2017, 50(4): 115-127.
Citation: LI Junsheng, XU Dong, LANG Zhen, et al. The Fluid Inclusion Characteristics and Significance of the Huaishuping Gold Depositin Song County, Henan province[J]. Northwestern Geology, 2017, 50(4): 115-127.
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The Fluid Inclusion Characteristics and Significance of the Huaishuping Gold Depositin Song County, Henan province

  • 1. No.2 Institute of Geological & Mineral Resources Survey of Henan, Zhengzhou 450002, Henan, China;

  • 2. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, Henan, China;

  • 3. No.3 Institute of Geological & Mineral Resources Survey of Henan Geological Bureau, Xinyang 464000, Henan, China

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  • Received Date: October 04, 2016
  • Revised Date: July 25, 2017
  • Available Online: July 28, 2022
  • Published Date: December 04, 2017
    Graphical Abstract
    • Abstract
  • The Huaishuping gold deposit is a quartz vein gold deposit, which was occurred in slowly inclined interlayer extrusion zone of Xiong'er Group. Hydrothermal ore-forming process of this deposit can be divided into three stages:stage Ⅰ-milky quartz vein-phase crumb pyrite quartz vein, stage Ⅱ-smoke gray-polymetallic sulfide phase, and stage Ⅲ-quartz-carbonate phase. Through the studies of fluid inclusion microscopic temperature measurement and Laser-Raman spectra analysis, the results show that:three types of fluid inclusions in stage Ⅰ and Ⅱ are identified as CO2-H2O type, pure CO2 and NaCl-H2O solution type,while stage Ⅲ quartz inclusions main contain the NaCl-H2O solution type. From the metallogenic stage Ⅰ to stage Ⅲ, the homogenization temperatures of fluid inclusions are 189~439℃→145~351℃→145~267℃, while their salinities are 6.98%~10.29%→2.03%~11.71%→2.89%~15.04%. The ore-forming fluid was evolved from H2O-NaCl-CO2 system,which is characterized by changing from medium temperature and medium-low salinity to low temperature and salinity NaCl-H2O system. It's determined that the ore-forming fluid was derived from magmatic hydrothermal, which has the characteristics of deep source. And then, it's suggested that the ore-forming fluid was mainly migrated in the form of Au (HS), secondly by Au2(HS)2S2-.
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