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LIU Zhengyi, WANG Shengyun, GU Dazhao, et al. Discussion on the Characteristics of Ore-bearing Rock and the Genesis of the Jiling Uranium Deposit[J]. Northwestern Geology, 2018, 51(2): 160-170.
Citation: LIU Zhengyi, WANG Shengyun, GU Dazhao, et al. Discussion on the Characteristics of Ore-bearing Rock and the Genesis of the Jiling Uranium Deposit[J]. Northwestern Geology, 2018, 51(2): 160-170.
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Discussion on the Characteristics of Ore-bearing Rock and the Genesis of the Jiling Uranium Deposit

  • 1. Beijing Research Institute of Uranium Geology, Beijing 100029, China;

  • 2. China National Nuclear Corporation, Beijing 100045, China

More Information
  • Received Date: November 27, 2017
  • Revised Date: December 19, 2017
  • Available Online: July 28, 2022
  • Published Date: June 04, 2018
    Graphical Abstract
    • Abstract
  • The Longsushan magmatic activity belt is a uranium metallogenic belt characterized by typical alkali-metasomatite uranium. The large ore deposit is always closely related to alkali-metasomatism. The Jiling uranium deposit is attributed to Galedonian-Variscan magmatic hydrothermal fluids related to subduction. The Galedonian and Hercynian granites are respectively the products of northward and intracontinental subduction of Qilian ocean plate. According to the long-term field study and indoor comprehensive analysis (including microexamination, trace element and isotopic measurement), the characteristics of ore bearing rock and the genesis of the Jiling uranium deposit have been summarized in this paper.
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    • References (45)
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