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    Volume 43 Issue 9
    Sep.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(9): 3218-3233
    Li Shijie, Wei Qirong, Ci Qiong, Deng Xiaojun, Zheng Qiuping, Lu Haodong, Ji Xuefeng, Wang Jian, Xu Huan, Yang Changqing, 2018. Geochronology, Petrogeochemistry and Petrogenesis of Ore-Bearing Rock Massif in Dabu Mining Area, Tibet. Earth Science, 43(9): 3218-3233. doi: 10.3799/dqkx.2018.231
    Citation: Li Shijie, Wei Qirong, Ci Qiong, Deng Xiaojun, Zheng Qiuping, Lu Haodong, Ji Xuefeng, Wang Jian, Xu Huan, Yang Changqing, 2018. Geochronology, Petrogeochemistry and Petrogenesis of Ore-Bearing Rock Massif in Dabu Mining Area, Tibet. Earth Science, 43(9): 3218-3233. doi: 10.3799/dqkx.2018.231
    shu

    Geochronology, Petrogeochemistry and Petrogenesis of Ore-Bearing Rock Massif in Dabu Mining Area, Tibet

    doi: 10.3799/dqkx.2018.231
    • 1.

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

    • 2.

      No.2 Geological Party, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Lhasa 850000, China

    • 3.

      No. 404 Geological Team, Sichuan Bureau of Geology and Mineral Resources, Xichang 615000, China

    • 4.

      Henan Institute of Geological Survey, Zhengzhou 450001, China

    • Received Date: 2018-04-09
    • Publish Date: 2018-09-15
      Abstract
    • Dabu mining area is located in the southern part of the middle Gangdese metallogenic belt, which has great metallogenic potential of Cu (Mo) deposit. In this paper, petrology, LA-ICP-MS zircon U-Pb dating, rock geochemistry of the Dabu ore-bearing granodiorite body are systematically studied. The results suggest that the Dabu granodiorite pluton is one of the major ore-bearing rock body, and its LA-ICP-MS zircon U-Pb age is 16.5±0.3 Ma-16.0±0.4 Ma, with the corresponding age of Miocene (N1). The rock mass has high Al (Al2O3=15.6%-16.5%), high Na (Na2O=4.51%-4.82%), and it is calc-alkaline and weakly peraluminous. REE elements have weak positive Eu anomalies (Eu/Eu*=1.02-1.27) and positive Ce anomalies (Ce/Ce*=0.99-1.53). Trace elements ratio spider diagram displays apparent enrichments of Rb, Ba, Sr and marked depletions of Nb, Ta, Ti, Y. The Dabu granodiorite pluton belongs to Ⅰ-type granite, which is similar to the typical C-type adakite, but is obviously different from the Miocene high-K adakite in the Gangdese belt. It is concluded that Dabu granodiorite pluton is a relatively high degree of partial melting of the thickened lower crust material (garnet amphibolite) formed in the background of partial extension of the India Asian continent post-collision.

       

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