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    Volume 47 Issue 8
    Sep.  2022
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    Article Navigation >  Earth Science  > 2022  >  47(8): 2889-2901
    Zhang Peichun, Peng Bo, Zhao Jinzhong, Wang Xin, He Ji, Zhang Ai, Shuang Long, 2022. Petrogenesis of the Syenogranite in the Xiaowulangou Area of Southern Great Xing'an Range: Constraints from Zircon LA⁃ICP⁃MS U⁃Pb Geochronology, Geochemistry and Hf Isotopes. Earth Science, 47(8): 2889-2901. doi: 10.3799/dqkx.2021.129
    Citation: Zhang Peichun, Peng Bo, Zhao Jinzhong, Wang Xin, He Ji, Zhang Ai, Shuang Long, 2022. Petrogenesis of the Syenogranite in the Xiaowulangou Area of Southern Great Xing'an Range: Constraints from Zircon LA⁃ICP⁃MS U⁃Pb Geochronology, Geochemistry and Hf Isotopes. Earth Science, 47(8): 2889-2901. doi: 10.3799/dqkx.2021.129
    shu

    Petrogenesis of the Syenogranite in the Xiaowulangou Area of Southern Great Xing'an Range: Constraints from Zircon LA⁃ICP⁃MS U⁃Pb Geochronology, Geochemistry and Hf Isotopes

    doi: 10.3799/dqkx.2021.129
    • 1.

      MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Science, Beijing 100037, China

    • 2.

      Inner Mongolia Key Laboratory of Magmatic Mineralization and Ore-Prospecting, Inner Mongolia Geological Survey Institute, Hohhot 010020, China

    • 3.

      Inner Mongolia Minerals Experiment Research Institute, Hohhot 010031, China

    • Received Date: 2021-05-24
    • Publish Date: 2022-09-25
      Abstract
    • TheLate Jurassic⁃Early Cretaceous granites are widely developed in the west slop of Southern Great Xing'an Range, and an in⁃depth study of the petrogenesis is of great geological significance to reveal the Mesozoic geodynamic background and tectonic evolution. In this paper, we report for the zircon LA⁃ICP⁃MS U⁃Pb age and Hf isotopic data, whole⁃rock major and trace element composition data from Xiaowulangousyeno granite. LA⁃ICP⁃MS U⁃Pb dating yields a weighted mean of 139.4±0.7 Ma, indicating that Xiaowulangousyeno granite formed in the Early Cretaceous. Geochemically, the syenogranite belongs to Si⁃K⁃rich calc⁃alkaline series, A/CNK=1.00~1.11 and are weak peraluminous. The syenogranite enriched in Rb, Th, U(LILE) and light rare earth elements(LREE), relatively depleted in Ba, Sr, P, Ti(HFSE), withobvious Eu negative anomaly(δEu=0.007~0.009). In addition, the (Zr+Nb+Ce+Y) values of syenograniteis less than 350×10⁃6. The syenogranite contains magnetite, and no primary muscovite and alkaline mafic minerals. All these features above suggest that Xiaowulangousyenogranite belongs to highly fractionated Ⅰ⁃type granite. The zircons εHf(t) values of syenogranite are +5.5~+8.9, and the two stage model ages (tDM2) range 700 Ma to 947 Ma. Combined with the reginoal geological background, we conclude that the Xiaowulangousyenograniteoriginated from the partial melting of upper Proterozoic meta⁃mafic rocks and middle Ordovician meta⁃andesite rocks under low pressure and high temperature, and the syenogranitewas the product of extension after the closure of Mongol⁃Okhotsk Ocean.

       

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