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    KANG Cong-xuan, ZONG Wen, XIAO Yuan-fu, et al. Mineralization Model for Tangbula Porphyry-Type Mo (Cu) Deposit in East Gangdisi, Tibet[J]. Northwestern Geology, 2013, 46(3): 83-89.
    Citation: KANG Cong-xuan, ZONG Wen, XIAO Yuan-fu, et al. Mineralization Model for Tangbula Porphyry-Type Mo (Cu) Deposit in East Gangdisi, Tibet[J]. Northwestern Geology, 2013, 46(3): 83-89.
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    Mineralization Model for Tangbula Porphyry-Type Mo (Cu) Deposit in East Gangdisi, Tibet

    • 1.

      Nanjing Center of Geological Survey, Nanjing 210016, China

    • 2.

      College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

    • 3.

      Tibetan Bureau of Geology and Exploration of Mineral Resources, Lasa 850000, China

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    • Received Date: March 17, 2013
    • Revised Date: May 14, 2013
    • Published Date: September 04, 2013
      Graphical Abstract
      • Abstract
    • Located east to Gangdisi tectonic metallogenic belt, Tangbula porphyry-type Mo (Cu) deposit boasts advantageous metallogenic conditions. The article analyzed the geological background of mineralization, the time of digenesis and mineralization, the source of ore-forming materials, the process of mineralization, the state of orebodies occurrence, and finally established a metallogenic model. Results have shown that the digenesis and mineralization of Gangdisi porphyry-type copper deposit occurred intensively in the Himalayan period, the formation is related to the northward subduction of Tethyan oceanic crust into the bottom of the Lhasa terrane. The ore-bearing rock are mainly intrusive rocks of intermediate acid calc-alkaline rock series with characteristics of adakitic rock. The mineralization pattern is of practical significance to regional mineralization forecast and metallogenic model establishment.
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