Volume 43 Issue 12
Dec.  2018
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Article Navigation >  Earth Science  > 2018  >  43(12): 4606-4620
Li Huan, Li Yanjun, Wei Junhao, Shi Wenjie, Li Hongmei, 2018. Rb-Sr Isochron Age of Auriferous Pyrites from Dunbasitao Gold Deposit in East Junggar, Xinjiang, and Its Geological Significance. Earth Science, 43(12): 4606-4620. doi: 10.3799/dqkx.2018.988
Citation: Li Huan, Li Yanjun, Wei Junhao, Shi Wenjie, Li Hongmei, 2018. Rb-Sr Isochron Age of Auriferous Pyrites from Dunbasitao Gold Deposit in East Junggar, Xinjiang, and Its Geological Significance. Earth Science, 43(12): 4606-4620. doi: 10.3799/dqkx.2018.988
shu

Rb-Sr Isochron Age of Auriferous Pyrites from Dunbasitao Gold Deposit in East Junggar, Xinjiang, and Its Geological Significance

doi: 10.3799/dqkx.2018.988
  • 1.

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

  • 2.

    National Demonstration Center for Experiment of Mineral Exploration Education, Wuhan 430074, China

  • 3.

    Hubei Geological Survey, Wuhan 430034, China

  • Received Date: 2018-06-06
  • Publish Date: 2018-12-15
    Abstract
  • The study on direct dating of ore minerals in gold deposits in East Junggar is relatively scarce. The Dunbasitao gold deposit, located in the northeastern part of eastern Aermantai structural belt, is one of typical gold deposits in the region. Rb-Sr isotopic dating of 9 pyrites separated from the Dunbasitao gold deposit yielded an isochron age of 268.3±2.8 Ma (MSWD=0.7), and this result is in good agreement with the high-potassium calc-alkaline granite in the northwestern part of ore district, indicating that gold mineralization was related to granite crystallization.Meanwhile, combining with the studies about metallogenic chronology of diagenetic and mineralization in East Junggar in recent years, it is suggested that Middle Permian from 270 Ma to 260 Ma may be an important time range of gold mineralization in East Junggar, Xinjiang. According to previous studies and the Rb-Sr ages reported, it is interpreted that the Dunbasitao gold deposit was formed in an post-collision extended environment related to lithospheric extension with tectonic, magma and fluid activities during the Middle Permian in East Junggar. The age of Dunbasitao gold deposit reported in this study is of great significance both for comparison studies in minerization of gold deposits in the region and practice for mineral exploration.

     

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