Volume 25 Issue S1
May  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(S1): 39-43
ZHANG Zhi, QI Fanyu, ZHEN Shimin, 2019. THE CHARACTERISTICS OF ORE-CONTROLLING STRUCTURE IN THE BAOSHAN CU-PB-ZN POLYMETALLIC DEPOSIT, HUNAN PROVINCE. Journal of Geomechanics, 25 (S1): 39-43. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.007
Citation: ZHANG Zhi, QI Fanyu, ZHEN Shimin, 2019. THE CHARACTERISTICS OF ORE-CONTROLLING STRUCTURE IN THE BAOSHAN CU-PB-ZN POLYMETALLIC DEPOSIT, HUNAN PROVINCE. Journal of Geomechanics, 25 (S1): 39-43. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.007
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THE CHARACTERISTICS OF ORE-CONTROLLING STRUCTURE IN THE BAOSHAN CU-PB-ZN POLYMETALLIC DEPOSIT, HUNAN PROVINCE

doi: 10.12090/j.issn.1006-6616.2019.25.S1.007

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

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  • Published: 2019-05-01
    Abstract
  • The Baoshan Cu-Pb-Zn polymetallic deposit is located in the northern margin of the middle section in the Nanling metallogenic belt. It is divided into the middle skarn type copper-molybdenum ore and the peripheral hydrothermal type lead-zinc-silver deposit. It has typical zoning characteristics. The ore body orientation is controlled by structure. According to the occurrence of ore bodies, it can be seen that the formation of Baoshan copper-lead-zinc polymetallic deposits is multi-stage. The ore-controlling structure of the skarn formation period is the F0 fault, and the ore-controlling structure during the metal sulfide formation period is the F21 and F25 faults. The F0, F21 and F25 faults are the main channels for ore-bearing hydrothermal migration, and the inverted anticline and syncline structure provide a good space for the rich ore containing ore-bearing hydrothermal fluid.

     

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