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Geoscience ›› 2021, Vol. 35 ›› Issue (06): 1622-1632.DOI: 10.19657/j.geoscience.1000-8527.2021.106

• Gold-polymetallic Mineralization in Qinling Orogens • Previous Articles     Next Articles

Pyrite Trace Element, Hydrogen, Oxygen, and Sulfur Isotope Geochemistry of the Xiajiadian Gold Deposit in Zhashui-Shanyang Orefield, South Qinling Orogen, and Its Metallogenic Constraints

DING Kun1,2,3,4(), WANG Ruiting2,3,4(), LIU Kai5, WANG Zhihui1, SHEN Ximao6   

  1. 1. Shaanxi Railway Institute, Weinan,Shaanxi 714099, China
    2. Shaanxi Provincial Engineering and Technology Research Center for Comprehensive Utilization of Mineral Resources, Xi'an,Shaanxi 710054, China
    3. Northwest Geological Exploration for Nonferrous Metals, Xi'an,Shaanxi 710054, China
    4. School of Earth Science and Resources,Chang'an University, Xi'an,Shaanxi 710054, China
    5. No.713 Geological Team, Northwest Bureau of Geological Exploration for Nonferrous Metals, Shangluo,Shaanxi 726000,China
    6. Xi'an Northwest Research Institute of Nonferrous Metals Co.,Ltd., Xi'an,Shaanxi 710054, China
  • Received:2020-12-02 Revised:2021-10-20 Online:2021-12-10 Published:2022-02-14
  • Contact: WANG Ruiting

Abstract:

To clarify the genesis of Xiajiadian gold deposit in the Zhashui-Shanyang orefield, in-situ trace element, hydrogen, oxygen and sulfur isotope compositions of the ore pyrite and wallrock samples were analyzed by LA-(MC)-ICP-MS techniques. The results show that the pyrite Co/Ni ratio ranges from 0.11 to 0.76, indicating that it is sedimentary pyrite. The pyrite δ34S value (-9.40‰ to 7.16‰) is close to that of the carbonaceous slate wallrock (-8.84‰ to 10.64 ‰), whilst the average pyrite δ34S value (2.47‰) falls within the magmatic sulfur range, suggesting that the ore sulfur may have sourced from the mixing of sedimentary sulfur with magmatic sulfur. The hydrogen-oxygen isotope data show that the ore-forming fluid was principally originated from magmatic water, with meteoric water input in the late-stage mineralization. Evidence from geological characteristics, ore-forming temperature, gold occurrence and pyrite trace elements and sulfur isotopes suggest that the deposit belongs to Carlin-type. The ore-forming fluid may have come mainly from magmatic water with late-stage meteoric water input, featuring a crust-mantle mixed source.

Key words: ore genesis, sulfur isotope, trace element, Xiajiadian gold deposit, Zhashui-Shanyang orefield

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