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    Volume 43 Issue 8
    Aug.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(8): 2742-2754
    Liang Wei, Zhang Linkui, Xia Xiangbiao, Ma Guotao, Huang Yong, Zhang Zhi, Fu Jiangang, Cao Huawen, Miao Huaqing, Li Guangming, 2018. Geology and Preliminary Mineral Genesis of the Cuonadong W-Sn Polymetallic Deposit, Southern Tibet, China. Earth Science, 43(8): 2742-2754. doi: 10.3799/dqkx.2018.154
    Citation: Liang Wei, Zhang Linkui, Xia Xiangbiao, Ma Guotao, Huang Yong, Zhang Zhi, Fu Jiangang, Cao Huawen, Miao Huaqing, Li Guangming, 2018. Geology and Preliminary Mineral Genesis of the Cuonadong W-Sn Polymetallic Deposit, Southern Tibet, China. Earth Science, 43(8): 2742-2754. doi: 10.3799/dqkx.2018.154
    shu

    Geology and Preliminary Mineral Genesis of the Cuonadong W-Sn Polymetallic Deposit, Southern Tibet, China

    doi: 10.3799/dqkx.2018.154

    • Chengdu Center of China Geological Survey, Chengdu 610081, China

    • Received Date: 2018-03-05
    • Publish Date: 2018-08-15
      Abstract
    • Researchers have not paid attention to the tungsten-tin mineralization of the Tethys Himalayan lead-zinc-gold-metallogenic belt.The Cuonadong W-Sn polymetallic deposit is located in a newly recognized giant gneiss dome, eastern Tethys Himalaya.The deposit is rich in W, Sn and Be, accompanied by Cu, Pb, Zn, Bi and Mo, of which mineralization type is skarn-type. Besides, the mineralization of beryllium contains pegmatite type.Main ore minerals are scheelite, cassiterite and bertrandite, with minor chalcopyrite, galena, sphalerite, bismuthinite and molybdenited.There are also some zeunerite, uraninite and thorite, indicating the uranium mineralization potential.Geological survey shows that the Cuonadong W-Sn polymetallic deposit could be a large-or super large-scale ore deposit.Low concentration of Zr and relatively low ratios of Zr/Hf and Nb/Tb demonstrate that leucogranite within the Cuonadong dome is highly fractional crystallization.Meanwhile, there is absolutely little magnetite but relatively rich in ilmenite with Fe2O3/FeO < 0.5 and low Ce/Ce* ratio (average 23) in leucogranite, indicating characteristics of reductive granite.The reductive and highly fractional crystallization granite is a necessary condition for the formation of the tungsten-tin polymetallic deposit, additionally, the gneiss dome controls its spatial distribution.Therefore, the Cuonadong W-Sn polymetallic deposit is both controlled by dome structure and leucogranite.

       

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