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中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

世界期刊影响力指数报告Q1区（2023）

Volume 43 Issue 2
Mar.  2024
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Article Contents
Article Navigation >  Bulletin of Geological Science and Technology  > 2024  >  43(2): 156-174
YAN Ziqing, SHI Wenjie, ZHANG Pengtao, WANG Yongjun, SHAO Yubao, HUANG Xin, SONG Yu, TAN Jun, WANG Zhihua. Ore genesis and vertical variations of ore-forming fluids in the Dayingezhuang gold deposit, Jiaodong Peninsula: Constraints from fluid inclusions, ore forming elements, and H-O-S-Pb isotopes[J]. Bulletin of Geological Science and Technology, 2024, 43(2): 156-174. doi: 10.19509/j.cnki.dzkq.tb20220507
Citation: YAN Ziqing, SHI Wenjie, ZHANG Pengtao, WANG Yongjun, SHAO Yubao, HUANG Xin, SONG Yu, TAN Jun, WANG Zhihua. Ore genesis and vertical variations of ore-forming fluids in the Dayingezhuang gold deposit, Jiaodong Peninsula: Constraints from fluid inclusions, ore forming elements, and H-O-S-Pb isotopes[J]. Bulletin of Geological Science and Technology, 2024, 43(2): 156-174. doi: 10.19509/j.cnki.dzkq.tb20220507
shu

Ore genesis and vertical variations of ore-forming fluids in the Dayingezhuang gold deposit, Jiaodong Peninsula: Constraints from fluid inclusions, ore forming elements, and H-O-S-Pb isotopes

doi: 10.19509/j.cnki.dzkq.tb20220507
  • 1.

    School of Earth Resources, China University of Geosciences(Wuhan), Wuhan 430074, China

  • 2.

    Ecological Geology Brigade of Jiangxi Geological Bureau, Nanchang 330030, China

  • 3.

    Shandong Coalfield Geological Planning Investigation Institute, Jinan 250104, China

More Information
    Abstract
  • Objective

    The Dayingezhuang gold deposit in the middle of the Zhaoping metallogenic belt represents a typical altered-rock type deposit with a giant Au reserve of 283 tons on the Jiaodong Peninsula. The genetic type of the deposit is still controversial.

    Methods

    Based on detailed field observations, ore genesis and variations in ore-forming fluids from different depths were investigated in this study.

    Results

    Fluid inclusion studies show that the ore-forming fluids formed an H2O-CO2-NaCl±CH4 system with moderate temperature, low salinity, and moderate-low density. Furthermore, the temperatures and salinities decrease gradually from the early to late mineralization stages(Ⅰ-Ⅳ), but the opposite occurs at densities. Hydrogen and O isotopic compositions show that the ore fluids were dominated by magmatic water in the early stage, with subordinate meteoric water input during the late stages. Fluid boiling occurred possibly during the main mineralization stages. Sulfur and Pb isotopes of pyrite indicate that the ore-forming materials were derived from deep crust-mantle mixed magma. Overall, the mineralization process and tectonic setting are similar to those of the other Jiaodong gold deposits in a craton-destruction environment.

    Conclusion

    Comprehensive comparisons of ore fluids, Au and Ag contents, and gold fineness between shallow and deep ores show that ore fluids and mineralization intensity are consistent throughout the deposit. Gold precipitation has a broad and stable environment, indicating the great potential for mineral exploration in deep spaces.

     

    • The authors declare that no competing interests exist.
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