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WU Yi-ping, ZHANG Zhao-wei, ZHANG Xiao-mei, et al. Characteristics and Indicators of Gold Deposit in Gold-Bearing Silicon-Iron Formation on Northern Margin of Kunlun Mountains, Xinjiang[J]. Northwestern Geology, 2007, 40(4): 17-25.
Citation: WU Yi-ping, ZHANG Zhao-wei, ZHANG Xiao-mei, et al. Characteristics and Indicators of Gold Deposit in Gold-Bearing Silicon-Iron Formation on Northern Margin of Kunlun Mountains, Xinjiang[J]. Northwestern Geology, 2007, 40(4): 17-25.
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Characteristics and Indicators of Gold Deposit in Gold-Bearing Silicon-Iron Formation on Northern Margin of Kunlun Mountains, Xinjiang

  • 1.

    No.1 Team of Regional Geological Survey, Xinjiang Bureau of Geological Prospecting, Xinjiang 830011, China

  • 2.

    Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

  • 3.

    Chang'an University, Xi'an 547100, China

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  • Received Date: May 14, 2007
  • Revised Date: November 11, 2007
  • Published Date: December 04, 2007
    Graphical Abstract
    • Abstract
  • The gold deposit in gold-bearing silicon-iron formation has been a characteristic deposit type found in the Kunlun mountains in recent years.Based on detailed geologicalwork, a number of gold ore deposits such as the Paximu,the Ku'a-Qiakenengsayi and the Mate deposits have been successively found in the area.The depositsoccur in theAqiang Formation that is a gold-bearing silicon-iron formation in the marine volcanic eruption-normal clastic deposition foamed in exhalative-sedimentation setting.Regionally, the deposits have clear features of strata-bound ore deposit, which is sinilar to the "Dongfengshan type" in Heilongjiang province.The ore genesis belongs to the type of sedimentary-metamorphic reworking related to volcanic-sedimentary processes.
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    • References (22)
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