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    Volume 44 Issue 7
    Jul.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(7): 2265-2274
    Dong Suiliang, Zhang Zhi, Li Guangming, Zhang Linkui, Huang Yong, Fu Jiangang, Fang Ming, 2019. Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance. Earth Science, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099
    Citation: Dong Suiliang, Zhang Zhi, Li Guangming, Zhang Linkui, Huang Yong, Fu Jiangang, Fang Ming, 2019. Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance. Earth Science, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099
    shu

    Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance

    doi: 10.3799/dqkx.2019.099
    • 1.

      Chengdu Center, China Geological Survey, Chengdu 610081, China

    • 2.

      Hubei Geological Survey, Wuhan 430034, China

    • Received Date: 2019-04-03
    • Publish Date: 2019-07-15
      Abstract
    • The Gangqiongla Mo-Cu deposit is a newly discovered quartz vein type Mo-Cu deposit in the eastern Gangdise metallogenic belt. This paper first presents the Re-Os geochronology of molybdenite in the Gangqiongla quartz vein Mo-Cu deposit. Eight molybdenite samples from the quartz vein molybdenite yielded a weighted average age of 22.6±0.2 Ma(MSWD=1.3)and an isochron age of 24.1±1.3 Ma (MSWD=1.1), which is interpreted to represent the age of main stage ore, and is earlier than the age ranging from 17 Ma to 12 Ma of other porphyry Cu-Mo mineralization in the southern Gangdise metallogenic belt. The Re contents on molybdenite samples range from 239.1×10-6 to 314.7×10-6, suggesting that mantle materials more or less contribute to the main stage mineralization. Based on the Oligocene-Early Miocene regional mineralization data, the formation of Gangqiongla Mo-Cu deposit was associated with the Early Miocene transition stage from collision to extension between the India and Eurasia continents.

       

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