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Geoscience ›› 2021, Vol. 35 ›› Issue (06): 1587-1596.DOI: 10.19657/j.geoscience.1000-8527.2021.115

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

Sulfur and Lead Isotope Compositions of the Xiaohe Gold Deposit at Xunyang, Shaanxi Province, and Its Geological Significance

MENG Wuyi1(), LIU Jiajun2,3, WEI Liyong1, ZHANG Zhen1, WU Huanhuan1,2,3, FAN Baocheng1, PAN Yuan1, LI Guoying1, JIA Bin1   

  1. 1. Xi'an Center of Mineral Resources Survey, China Geological Survey, Xi'an,Shaanxi 710100, China
    2. State Key Laboratory of Geological Processes and Mineral Resource, China University of Geosciences, Beijing 100083, China
    3. School of Earth Sciences and Resources,China University of Geosciences, Beijing 100083, China
  • Received:2021-06-04 Revised:2021-11-01 Online:2021-12-10 Published:2022-02-14

Abstract:

The Xiaohe is a medium-sized gold deposit discovered in the central belt of the South Qinling Orogen in recent years. The ores are fine-disseminated, and the orebodies are controlled by both strata and structures. Based on field work, four metallogenic stages are divided according to mineral assemblages and crosscutting relationships: Ⅰ. Quartz veins with little sulfide in early-ore-stage; Ⅱ. Quartz veins with main-ore-stage pyrite and arsenopyrite in main mineralization stage; Ⅲ. Quartz veins with main-ore-stage polymetallic sulfides; Ⅳ. Late-ore-stage calcite and quartz veins. Stage Ⅱ and Ⅲ are the main gold mineralization stages. In situ sulfur isotope analysis show that the δ34S value of stage Ⅰ pyrite=20.80‰-25.77‰ (avg.23.59‰), stage Ⅱ pyrite and arsenopyrite=15.46‰-19.12‰ (avg.17.5‰), stage Ⅲ galena and sphalerite=11.35‰-16.78‰ (avg.13.88‰). This indicates that the sulfur is mainly sedimentary-sourced, and there is continuous addition of low-δ34S hydrothermal fluid during the ore-forming process. The sulfide Pb isotope analysis yielded 206Pb/204Pb=17.882,1-18.367,4, 207Pb/204Pb=15.614,0-15.674,1, and 208Pb/204Pb=38.016,3-38.934,2, indicating that the lead was derived mainly from the crust with certain mantle input. Based on the deposit geological and S and Pb isotope characteristics, we suggest that fluid mixing occurred in the Xiaohe gold mineralization.

Key words: Xiaohe gold deposit, metallogenic stage, sulfur isotope, lead isotope, south Qinling Orogen

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