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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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