Volume 25 Issue 2
Apr.  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(2): 187-197
WANG Mingzhi, HAN Runsheng, ZHOU Wei, et al., 2019. ORE-FORMING STRUCTURE ANALYSIS OF THE LIANGYAN LEAD-ZINC MINING AREA IN NORTHWESTERN GUIZHOU DEPOSIT CONCENTRATION DISTRICT, CHINA. Journal of Geomechanics, 25 (2): 187-197. DOI: 10.12090/j.issn.1006-6616.2019.25.02.017
Citation: WANG Mingzhi, HAN Runsheng, ZHOU Wei, et al., 2019. ORE-FORMING STRUCTURE ANALYSIS OF THE LIANGYAN LEAD-ZINC MINING AREA IN NORTHWESTERN GUIZHOU DEPOSIT CONCENTRATION DISTRICT, CHINA. Journal of Geomechanics, 25 (2): 187-197. DOI: 10.12090/j.issn.1006-6616.2019.25.02.017
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ORE-FORMING STRUCTURE ANALYSIS OF THE LIANGYAN LEAD-ZINC MINING AREA IN NORTHWESTERN GUIZHOU DEPOSIT CONCENTRATION DISTRICT, CHINA

doi: 10.12090/j.issn.1006-6616.2019.25.02.017
  • 1.

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

  • 2.

    Southwest Institute of Geological Survey, Geological Survey Center for Non-ferrous Mineral Resources, Kunming 650093, Yunnan, China

  • 3.

    Guiyang Mining Investment & Development Corporation. Ltd., Guiyang 550002, Guizhou, China

More Information
  • Received: 2018-10-28
  • Revised: 2019-01-10
  • Published: 2019-04-01
    Abstract
  • The Liangyan Pb-Zn deposit is one of the typical deposits in the northwest Guizhou Pb-Zn polymetallic ore-concentrated area in the Sichuan-Yunnan-Guizhou Triangle area (SYGT). Based on detailed analysis of the ore-controlling structures of the three levels at DaJie ore section by Geological Mechanics Theory and Method of Ore-field, combining comprehensive analysis of regional structure, this paper focuses on the prospecting direction in the deeper part of this area. The analysis shows that at least three tectonic stages developed in this area, and the corresponding principal compressive stress changes successively from NW to NE, then to EW. Ore bodies controlled by different mechanisms occurred in different parts of the fault. It is concluded that the deposit was controlled by NW-SE-trending compressive stress processes in the ore-forming period, which is coincident to the tectonic stress field of the northeast Yunnan HZT deposit concentration district. This new understanding is different from the previous opinion that the Yadu-Mongdong metallogenic belt in the metallogenic period was controlled by NE-SW-trending compressive stress processes. The NW-SE-W compression is basically a tectonic event after the mineralization.

     

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