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    Volume 42 Issue 10
    Oct.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(10): 1684-1696
    Li Peng, Li Jiankang, Pei Rongfu, Leng Shuangliang, Zhang Xu, Zhou Fangchun, Li Shengmiao, 2017. Multistage Magmatic Evolution and Cretaceous Peak Metallogenic Epochs of Mufushan Composite Granite Mass: Constrains from Geochronological Evidence. Earth Science, 42(10): 1684-1696. doi: 10.3799/dqkx.2017.114
    Citation: Li Peng, Li Jiankang, Pei Rongfu, Leng Shuangliang, Zhang Xu, Zhou Fangchun, Li Shengmiao, 2017. Multistage Magmatic Evolution and Cretaceous Peak Metallogenic Epochs of Mufushan Composite Granite Mass: Constrains from Geochronological Evidence. Earth Science, 42(10): 1684-1696. doi: 10.3799/dqkx.2017.114
    shu

    Multistage Magmatic Evolution and Cretaceous Peak Metallogenic Epochs of Mufushan Composite Granite Mass: Constrains from Geochronological Evidence

    doi: 10.3799/dqkx.2017.114
    • 1.

      Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China

    • 2.

      Hubei Geological Survey, Wuhan430034, China

    • 3.

      311 Brigade of Hunan Nuclear Geology, Changsha410011, China

    • 4.

      Hunan Geological Survey, Changsha410116, China

    • Received Date: 2017-05-05
    • Publish Date: 2017-10-18
      Abstract
    • The differentiation process of granitic magma is an important factor constraining the metallogenic mechanism of rare metal. The superimposition of multistage magmatic activities in orogenic process could easily lead to the accumulation of metallogenic pegmatite melts. Mufushan composite granite mass, which is composed of multistage granite intrusions, formed an important rare metal ore concentration area in South China. In this paper we report muscovite 40Ar/39Ar dating results from tantalite-bearing muscovite albite pegmatite of Duanfengshan on the margin of granite mass, and beryl-bearing muscovite albite pegmatite of Daxing in its central region. The 40Ar/39Ar ages of muscovite are 127.7±0.9 Ma and 130.5±0.9 Ma. Based on the detailed field work and existing regional isotope chronological data, it is suggested that this area experienced long-lasting multistage magmatic evolution from early to middle Yanshanian. Rare metal mineralization of pegmatite occurred at the end of magmatic activities in Cretaceous, which showed the process of gradual enrichment and mineralization of rare metal led by regional multistage magmatic differentiation and evolution. These geological phenomena showed that Mufushan area has undergone a widely distributed continental collision orogeny in Indosinian and its tectonic setting shifted from continental collision to extensional thinning at Yanshanian. The multistage magmatic activities associated with regional lower crustal melting, which caused by underplating of basaltic magma during the process of lithospheric extension, led to the final rare metal mineralization.

       

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