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    Volume 41 Issue 1
    Jan.  2016
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    Article Navigation >  Earth Science  > 2016  >  41(1): 55-66
    Liu Jinlong, Sun Fengyue, Zhang Yajing, Ma Fang, Liu Fengxu, Zeng Le, 2016. Zircon U-Pb Geochronolog, Geochemistry and Hf Isotopes of Nankouqian Granitic Intrusion in Qingyuan Region, Liaoning Province. Earth Science, 41(1): 55-66. doi: 10.3799/dqkx.2016.004
    Citation: Liu Jinlong, Sun Fengyue, Zhang Yajing, Ma Fang, Liu Fengxu, Zeng Le, 2016. Zircon U-Pb Geochronolog, Geochemistry and Hf Isotopes of Nankouqian Granitic Intrusion in Qingyuan Region, Liaoning Province. Earth Science, 41(1): 55-66. doi: 10.3799/dqkx.2016.004
    shu

    Zircon U-Pb Geochronolog, Geochemistry and Hf Isotopes of Nankouqian Granitic Intrusion in Qingyuan Region, Liaoning Province

    doi: 10.3799/dqkx.2016.004
    • 1.

      College of Earth Sciences, Jilin University, Changchun 130061, China

    • 2.

      Jilin Province Geological Data Resources House, Changchun 130061, China

    • Received Date: 2015-08-30
    • Publish Date: 2016-01-15
      Abstract
    • LA-ICP-MS zircon U-Pb dating and geochemical data of the Nankouqian granitic intrusion were studied to determine its formation time and tectonic background. The zircon U-Pb dating results indicate that the granitic pluton was formed in the Late Triassic (224±1 Ma). The granite shows calc-alkaline and metaluminous to weakly peraluminous affinities, with A/CNK ratio ranging from 0.98 to 1.07. The granitic pluton has features similar to adakitic rock with high Sr (394×10-6-545×10-6) and low Yb (0.61×10-6-0.93×10-6). The in situ zircon εHf(t) value varies from -13.2 to -6.9, and a two-stage model age (TDM2) varies from 1 669 to 1 825 Ma. These characteristics suggest that the primary magma was derived from partial melting of primarily Proterozoic lower crustal materials. Considering the regional tectonic evolution, we suggest the granites formed in the post-orogenic extension setting which could be related to the closure of the Paleo-Asian Ocean.

       

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