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    中国百强科技报刊

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    Volume 36 Issue 2
    Mar.  2011
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    Article Navigation >  Earth Science  > 2011  >  36(2): 289-298
    LI Yan-jun, WEI Jun-hao, WU Gang, TAN Jun, JIANG Yong-jian, FU Le-bing, QU Wen-jun, LOU Wang-ping, XIE Chang-cai, 2011. Re-Os Dating of Molybdenite from the Maoduan Lead-Zinc Polymetallic Deposit in Southwestern Zhejiang Province and Its Geological Significance. Earth Science, 36(2): 289-298. doi: 10.3799/dqkx.2011.030
    Citation: LI Yan-jun, WEI Jun-hao, WU Gang, TAN Jun, JIANG Yong-jian, FU Le-bing, QU Wen-jun, LOU Wang-ping, XIE Chang-cai, 2011. Re-Os Dating of Molybdenite from the Maoduan Lead-Zinc Polymetallic Deposit in Southwestern Zhejiang Province and Its Geological Significance. Earth Science, 36(2): 289-298. doi: 10.3799/dqkx.2011.030
    shu

    Re-Os Dating of Molybdenite from the Maoduan Lead-Zinc Polymetallic Deposit in Southwestern Zhejiang Province and Its Geological Significance

    doi: 10.3799/dqkx.2011.030
    • 1.

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

    • 2.

      National Research Center of Geoanalysis, Beijing 100037, China

    • 3.

      No.7 Geological Team of Zhejiang Province, Lishui 323000, China

    • Received Date: 2010-03-07
    • Publish Date: 2011-03-01
      Abstract
    • The Maoduan lead-zinc polymetallic deposit, located in uplift area between the Jiangshan-Shaoxing and Zhenghe-Dabu deep faults in southwestern Zhejiang Province, is one of typical lead-zinc polymetallic deposits in this region. Re-Os dating of 5 molybdenite separated from the Maoduan lead-zinc polymetallic deposit gave model ages from 138.6±2.0 Ma to 140.0±1.9 Ma. These data yielded an isochron age of 137.7±2.7 Ma with MSWD=0.7, and a weighted average model age of 139.0±0.8 Ma (MSWD=0.5). This result is in good agreement with the Maoduan concealed monzogranite, indicating that Pb-Zn polymetal mineralization was related to granite crystallization. According to the precise Re-Os ages we have reported and previous studies, we interpret the Maoduan Pb-Zn deposit formed in an extensional setting related to lithospheric extension during the Early Cretaceous in South China. Meanwhile, we also point out that 140±7 Ma may be another important time range of tungsten-molybdenite-lead-zinc polymetallic mineralization in South China.

       

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