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    Volume 35 Issue 4
    Jul.  2010
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    LIN Guang-chun, 2010. Zircon U-Pb Age and Petrochemical Characteristics of Shimian Granite in Western Sichuan: Petrogenesis and Tectonic Significance. Earth Science, 35(4): 611-620. doi: 10.3799/dqkx.2010.076
    Citation: LIN Guang-chun, 2010. Zircon U-Pb Age and Petrochemical Characteristics of Shimian Granite in Western Sichuan: Petrogenesis and Tectonic Significance. Earth Science, 35(4): 611-620. doi: 10.3799/dqkx.2010.076

    Zircon U-Pb Age and Petrochemical Characteristics of Shimian Granite in Western Sichuan: Petrogenesis and Tectonic Significance

    doi: 10.3799/dqkx.2010.076
    • Received Date: 2009-10-26
      Available Online: 2021-11-10
    • Publish Date: 2010-07-01
    • Neoproterozoic magmatic rocks are widespread in western margin of the Yangtze block, and their genesis and tectonic setting have been an issue in hot debate at the present time. SHRIMP U-Pb zircon age, petrology, geochemical and Nd isotopic data are reported for the Neoproterozoic Shimian granite in the Kangdian rift of western Sichuan. This pluton is of metaluminous high-K calc-alkalic I-type granite and emplaced at 818±7 Ma. Petrology, geochemical and Nd isotopic characters suggest that the pluton was generated by partial melting of pre-existing, young (Late Mesoproterozoic to Early Neoproterozoic) island arc crust, with contamination of old crust materials during magma ascending and emplacement. The Shimian granite is the product of the tectonic transition from compression to introplate extension in western margin of the Yangtze block. Their arc-like geochemical features (such as Nb-Ta depletion) should have been inherited from the protoliths, rather than reflection of their tectonic setting when the pluton formed.

       

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