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    Volume 47 Issue 1
    Jan.  2022
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    Article Navigation >  Earth Science  > 2022  >  47(1): 368-386
    Zhou Liang, Hu Yuzhao, Tan Xiaolin, Li Piyou, Cheng Yong, 2022. Basin-Scale Structure of Pu'an Pb-Zn Deposit Area, Southwest Guizhou, China. Earth Science, 47(1): 368-386. doi: 10.3799/dqkx.2021.001
    Citation: Zhou Liang, Hu Yuzhao, Tan Xiaolin, Li Piyou, Cheng Yong, 2022. Basin-Scale Structure of Pu'an Pb-Zn Deposit Area, Southwest Guizhou, China. Earth Science, 47(1): 368-386. doi: 10.3799/dqkx.2021.001
    shu

    Basin-Scale Structure of Pu'an Pb-Zn Deposit Area, Southwest Guizhou, China

    doi: 10.3799/dqkx.2021.001
    • 1.

      Faculty of Land and Resources Engineering, Kunming University of Science and Technology, Kunming 650093, China

    • 2.

      Mineral Resources Prediction and Evaluation Engineering Laboratory of Yunnan Province, Kunming 650093, China

    • 3.

      Mining Engineering Faculty, Kunming Metallurgy College, Kunming 650093, China

    • Received Date: 2020-12-19
      Available Online: 2022-02-11
    • Publish Date: 2022-01-20
      Abstract

    • Pu'an Pb-Zn deposit area in Guizhou Province is situated in the Southwest Guizhou Depression on the northwest edge of South China fold belt. The ore bodies occur in the Carboniferous dolomitic limestone and dolomite, with significant characteristics of structural ore-control. Two-dimension (2D) seismic profile of the NW-SE striking passes through the Pb-Zn mine area, clearly revealing the stratum and NE-SW trending structural framework of the research area. From the shallow Devonian to the deep Neoproterozoic, a total of 3 seismic reflectors and 3 reflecting units are labeled. Based on recognition of two crucial surfaces of angular unconformity, the "2+1" basin stratigraphic framework consisting of double basement and single sedimentary cover is clearly represented, which provides new evidence for the tectonic attribute of Southwest Guizhou. The basin structural framework in the mining area is composed of two controlling thrust faults with secondary reverse faults and folds. Field observation and structural analysis of the fault outcrops and its secondary structures shown in the seismic profile were conducted, moreover the ore-controlling faults of 4 deposits were dissected. It is proposed that the Indosinian compressional deformation would be related to the ore-forming age. Based on the structural framework of the seismic interpretation, the role of each structural factor is detailed analysis in the mineralization process. The two deep-cut basement faults (first-order fault) would be fluid migration channels from atmospheric water and deep basin. The Guangxi unconformity would act as a lateral migration pathway. The thin-skin faults that cut across the Lower-Middle Devonian Huohong Formation (aquifuge) acted as a vertical migration conduit for ore-forming liquid to upward-rise to the Carboniferous mineralization. Combined with the structural ore-controlling characteristics of representative deposits, a model of basin-scale structural ore-controlling of the Pu'an lead-zinc study area was established.

       

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