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    中国百强科技报刊

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    Volume 44 Issue 7
    Jul.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(7): 2207-2223
    Xia Xiangbiao, Li Guangming, Cao Huawen, Liang Wei, Fu Jiangang, 2019. Petrogenic Age and Geochemical Characteristics of the Mother Rock of Skarn Type Ore Body in the Cuonadong Be-W-Sn Polymetallic Deposit, Southern Tibet. Earth Science, 44(7): 2207-2223. doi: 10.3799/dqkx.2019.038
    Citation: Xia Xiangbiao, Li Guangming, Cao Huawen, Liang Wei, Fu Jiangang, 2019. Petrogenic Age and Geochemical Characteristics of the Mother Rock of Skarn Type Ore Body in the Cuonadong Be-W-Sn Polymetallic Deposit, Southern Tibet. Earth Science, 44(7): 2207-2223. doi: 10.3799/dqkx.2019.038
    shu

    Petrogenic Age and Geochemical Characteristics of the Mother Rock of Skarn Type Ore Body in the Cuonadong Be-W-Sn Polymetallic Deposit, Southern Tibet

    doi: 10.3799/dqkx.2019.038

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

    • Received Date: 2018-12-31
    • Publish Date: 2019-07-15
      Abstract
    • The Cuonadong gneiss dome is a newly discovered dome in the North Himalaya gneiss domes (NHGD) belt. Mineralization of the Cuonadong super-large Be-W-Sn polymetallic deposit is developed in the Cuonadong dome. The Cuonadong Be-W-Sn polymetallic ore bodies exist in skarn, fractures and (giant) granite. The main genetic type of deposit is skarn type, and the mother rock of skarn type ore body is weakly oriented two-mica granite. In this paper, chronology and geochemical characteristics of metallogenic mother rock (weakly oriented two-mica granite) of skarn type ore body in the Cuonadong super-large Be-W-Sn polymetallic deposit are studied. Zircon U-Pb dating results show that the weakly oriented two-mica granite's formation time is 16.5±0.3 Ma, which belongs to magmatic activity of Miocene leucogranite. It shows that the Cuonadong super-large Be-W-Sn polymetallic deposit, which is the product of the extension stage of Himalayan collision orogenic process, was formed in Miocene. Geochemical data show that metallogenic mother rock (weakly oriented two-mica granite) is the calcium alkaline and strong peraluminous granite with high silica (73.36%-73.89%), low iron(0.96%-1.58%). Its total rare earth is relatively low, with enrichment of LREE, depletion of HREE and obvious negative Eu anomaly. The two-mica granite is characterized by an enrichment of some large iron lithophile elements (Rb, Th) and loss of high field strength elements (Zr, Ti).The geochemical characteristics of two-mica granite show that it is a set of highly fractionated leucogranite. The study shows that the weakly oriented two-mica granite may be the product of remelting of metaargillaceous rocks, which is closely related to the activities of the South Tibetan detachment system.

       

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