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2023 Vol. 50, No. 2
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ZHEN Shimin, ZHA Zhongjian, WANG Dazhao, LIU Jiajun, PANG Zhenshan, CHENG Zhizhong, XUE Jianling, WANG Jiang, BAI Haijun, LI Yang, CHEN Chao. 2023. Characteristics of ore-forming fluids of the Zhongshangou gold deposit, Zhangjiakou-Xuanhua area, Hebei Province: Limitation on the intrusive rock related telluride-gold deposits[J]. Geology in China, 50(2): 605-621. doi: 10.12029/gc20190927002
Citation: ZHEN Shimin, ZHA Zhongjian, WANG Dazhao, LIU Jiajun, PANG Zhenshan, CHENG Zhizhong, XUE Jianling, WANG Jiang, BAI Haijun, LI Yang, CHEN Chao. 2023. Characteristics of ore-forming fluids of the Zhongshangou gold deposit, Zhangjiakou-Xuanhua area, Hebei Province: Limitation on the intrusive rock related telluride-gold deposits[J]. Geology in China, 50(2): 605-621. doi: 10.12029/gc20190927002
shu

Characteristics of ore-forming fluids of the Zhongshangou gold deposit, Zhangjiakou-Xuanhua area, Hebei Province: Limitation on the intrusive rock related telluride-gold deposits

  • 1.

    Development and Research Center of China Geological Survey, Beijing 100037, China

  • 2.

    Technical Guidance Center for Mineral Resources Exploration, Ministry of Natural Resources, Beijing 100120, China

  • 3.

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

  • 4.

    State Key Laboratory of Nuclear Resource and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China

  • 5.

    Third Geological Brigade of Hebei Geological and Mineral Bureau, Zhangjiakou, 075000, Hebei, China

  • 6.

    College of Resources, Hebei GEO University, Shijiazhuang 050031, Hebei, China

    • Fund Project: Supported by the projects of China Geological Survey (No.DD20160052, No.DD20190570, No.DD20190159, No. DD20190166) and Hebei Provincial Natural Science Foundation (No.D2019403015, No.ZD2019003)
More Information
  • Author Bio: ZHEN Shimin, male, born in 1984, senior engineer, mainly engaged in mineral deposit science and deposit geochemistry research; E-mail: zhenshimin0001@163.com
Received Date:  27 September 2019
Revised Date:  16 August 2020
Publish Date:  25 April 2023
    Abstract

  • This paper is the result of mineral exploration engineering.

     Objective

    The Zhongshangou gold deposit is located in the north margin of North China Craton and the south side of Shangyi-Chongli-Chicheng deep fault. It is one of the typical gold deposits in Zhangjiakou-Xuanhua gold concentration area, Hebei Province. This paper discusses the characteristics and evolution of ore-forming fluids, in order to provide a theoretical basis for the exploration of the deposit.

     Methods

    This paper summarizes the regional mineralizing setting, geological characteristics of the mining area, ore body and ore characteristics. Representative samples from four metallogenic stages were selected to conduct research on fluid inclusion petrography and micro thermometry, hydrogen and oxygen isotopes, and helium and argon isotopes.

     Results

    The results indicate that it can be divided into four metallogenic stages: K-feldspar-pyrite-quartz stage (Ⅰ), milky white quartz-pyrite stage (Ⅱ), smoky gray quartz-sulfide stage (Ⅲ) and sulfide-poor-carbonate stage (Ⅳ). Gas-liquid two-phase primary fluid inclusions are mainly developed in each mineralization stage. The temperature measurement data of fluid inclusions show that the homogenization temperature and salinity of main ore-forming stage are respectively 210-250℃ and 6.01%-13.62%NaCleqv. Hydrogen and oxygen isotope show that δ18OH2O and δDV-SMOW values are respectively -2.97‰-6.96‰ and -94.6‰--80.2‰, which show that the δ18OH2O values drift to the atmospheric water line and show a linear change. Helium and argon isotope of the pyrite show that 3He/4He values are 1.82×10-7-9.24×10-7, 40Ar/36Ar values are 699.9-2200.4, R/Ra values are 0.13-0.66, radiogenic 40Ar* values are 55.89%-86.57%, and mantle derived helium values are 2.00%-10.86%.

     Conclusions

    The ore-forming fluid has experienced a continuous evolution process from medium-high temperature and medium-low salinity to low temperature and medium-low salinity. The main ore-forming stage experienced strong boiling. In the late stage of mineralization, there mixed in a large amount of meteoric water. With the development of mineralization, the proportion of mantle derived materials in mineralization increased gradually. The ore-forming fluid has the characteristics of magma fluid mixed with the crust and mantle. To sum up, the ore-forming fluid of Zhongshangou gold deposit is characterized by the intrusive rock related telluride-gold deposit.
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