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ZHONG Jiaxin, XU Gang, XIANG Liange, et al. Geological Characteristics and Metallogenetic Regularity of the Zhaobishan Iron Deposit in Beishan Area, Weining, Ningxia[J]. Northwestern Geology, 2018, 51(1): 228-237.
Citation: ZHONG Jiaxin, XU Gang, XIANG Liange, et al. Geological Characteristics and Metallogenetic Regularity of the Zhaobishan Iron Deposit in Beishan Area, Weining, Ningxia[J]. Northwestern Geology, 2018, 51(1): 228-237.
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Geological Characteristics and Metallogenetic Regularity of the Zhaobishan Iron Deposit in Beishan Area, Weining, Ningxia

  • 1. School of Geological Engineering and Mapping, Chang'an University, Xi'an 710054, Shannxi, China;

  • 2. Ningxia Institute of Survey and Monitoring of Land and Resources, Yinchuan 750004, Ningxia, China;

  • 3. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shannxi, China;

  • 4. Ningxia Institute of Geological Survey, Yinchuan 750021, Ningxia, China;

  • 5. No. 11 Gold Geological Party of the CAPF, Lasa 710100, Tibet, China

More Information
  • Received Date: September 29, 2017
  • Revised Date: November 21, 2017
  • Available Online: July 28, 2022
  • Published Date: March 04, 2018
    Graphical Abstract
    • Abstract
  • The iron deposits of Beishan area in Weining are mainly occurred in Devonian-Carboniferous clastic rocks, which are controlled by strata formation and tectonics.According to the characteristics of metallogenic geological background, mineral assemblage and wall rock alterations, these iron deposits in this area have been classified as the moderate-low temperature hydrothermal deposits.Due to its large reserves, numerous ore quantities, typical metallogenic background and ore genesis, the Zhaobishan iron deposit has a great significant to reveal the metallogenic geological characteristics, to carry out the comprehensive study, to establish the metallogenic models and to sum up the metallogenic regularities of the iron deposits in this area.
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    • References (27)
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