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WANG Yonglei, PEI Rongfu, LI Jinwen, WANG Haolin, LIU Xifeng. Geochemical Characteristics of Granites from the Jiangjunzhai Tungsten Deposit of Southeast Hunan Province and Its Re-Os Isotopic Dating[J]. Rock and Mineral Analysis, 2009, 28(3): 274-278.
Citation: WANG Yonglei, PEI Rongfu, LI Jinwen, WANG Haolin, LIU Xifeng. Geochemical Characteristics of Granites from the Jiangjunzhai Tungsten Deposit of Southeast Hunan Province and Its Re-Os Isotopic Dating[J]. Rock and Mineral Analysis, 2009, 28(3): 274-278.
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Geochemical Characteristics of Granites from the Jiangjunzhai Tungsten Deposit of Southeast Hunan Province and Its Re-Os Isotopic Dating

  • 1.

    Institute of Mineral Resources Chinese Academy of Geological Sciences

  • 2.

    Institute of Mineral Resources Chinese Academy of Geological Sciences

  • 3.

    Institute of Mineral Resources Chinese Academy of Geological Sciences

  • 4.

    Institute of Mineral Resources Chinese Academy of Geological Sciences

  • 5.

    Graduate School of China University of Geosciecnes

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  • Received Date: February 09, 2009
  • Revised Date: March 15, 2009
    Abstract
  • The Jiangjunzhai tungsten deposit is a typical quartz-wolframite deposit in Baiyunxian ore field. The granite body in the Jiangjunzhai tungsten deposit is a compound rockmass, which has the features of crust-derived type granite and is the product of comagmatic evolution. In this paper, the geochemical characteristics of granite in Jiangjunzhai tungsten deposit and the Re-Os isotopic dating of molybdenite from quartz-wolframite veins were studied and carried out, in order to elucidate the timing of mineralization and reveal the time limites and geodynamic setting of large-scale metallogeny in Southeast Hunan. Re-Os dating for four molybdenites yields a model age of (151.3±2.5) Ma～(163.6±2.3) Ma and an isochron age of (169.6±2.7) Ma, indicating that the Jiangjunzhai tungsten deposit was formed in the Early Yanshanian period and is the result of large scale mineralization in South China.
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