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    Volume 43 Issue 12
    Dec.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(12): 4269-4282
    Zha Xianfeng, Gao Xiaofeng, Li Ping, Ji Wenhua, 2018. Origin of Diabase Dykes in Mazar Area in West Kunlun Orogenic Belt: Evidences from Zircon U-Pb Dating and Geochemistry. Earth Science, 43(12): 4269-4282. doi: 10.3799/dqkx.2018.327
    Citation: Zha Xianfeng, Gao Xiaofeng, Li Ping, Ji Wenhua, 2018. Origin of Diabase Dykes in Mazar Area in West Kunlun Orogenic Belt: Evidences from Zircon U-Pb Dating and Geochemistry. Earth Science, 43(12): 4269-4282. doi: 10.3799/dqkx.2018.327
    shu

    Origin of Diabase Dykes in Mazar Area in West Kunlun Orogenic Belt: Evidences from Zircon U-Pb Dating and Geochemistry

    doi: 10.3799/dqkx.2018.327
    • 1.

      Xi'an Center of Geological Survey, Orogen Research Center, China Geological Survey, Xi'an 710054, China

    • 2.

      Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Xi'an 710054, China

    • Received Date: 2018-09-12
    • Publish Date: 2018-12-15
      Abstract
    • The West Kunlun orogenic belt underwent the tectonic process of Proto-and Paleo-Tethys Oceans since Phanerozoic. However, there is still much controversy over the evolution of the Paleo-Tethys Ocean. Geochemistry and zircon U-Pb and Hf isotopic compositions of the diabase dykes in Mazar, West Kunlun are reported in this paper. Zircon U-Pb dating results give an emplacement age of 287±4.6 Ma for the Mazar diabase. These rocks span a SiO2 range of 48.29%-50.21% and Mg# (0.36-0.39), characterized by moderate LREE/HREE fractionation, strong LILEs (such as Rb, Ba, Sr) enrichment and depleted Nb-Ta, P and weakly Eu depletion. They have more radiogenic zircon Hf isotopic compositions (εHf(t)=4.00-13.71, average value is 7.61) than N-MORB. In combination with the evolution of regional geology, it is suggested that these melts were derived from partial melting of an enriched lithospheric mantle that underwent early subducted fluid metasomatization. The origin of the Mazar diabase dykes indicates that the post-orogenic extension in West Kunlun, from Late Devonian to Early Permian, may be not related to the Tarim mantle plume.

       

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