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    中国百强科技报刊

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    Volume 35 Issue 6
    Jun.  2010
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    Article Navigation >  Earth Science  > 2010  >  35(6): 921-932
    LI Yi-long, ZHOU Han-wen, ZHONG Zeng-qiu, YIN Shu-ping, LI Fu-ling, 2010. Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia. Earth Science, 35(6): 921-932. doi: 10.3799/dqkx.2010.107
    Citation: LI Yi-long, ZHOU Han-wen, ZHONG Zeng-qiu, YIN Shu-ping, LI Fu-ling, 2010. Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia. Earth Science, 35(6): 921-932. doi: 10.3799/dqkx.2010.107
    shu

    Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia

    doi: 10.3799/dqkx.2010.107
    • 1.

      Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 2.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • 3.

      Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • Received Date: 2010-05-26
    • Publish Date: 2010-11-01
      Abstract
    • A large scale of intermediate dykes developed in Xar Moron fault belt in Linxi county, Inner-Mongolia, with NE3° to 5° angle of strike and nearly vertical trend. LA-ICP-MS zircon U-Pb dating method and whole rock geochemistry test were applied. It is indicated that the intermediate dykes emplaced in Lower Cretaceous with LA-ICP-MS zircon U-Pb age of 132.2±2.2Ma. The whole rock geochemistry of the dykes reveals transition characteristics between high potassium calc-alkaline series and shoshonite series. They formed in intraplate extensional background and sourced from crust-mantle magmatic mixing, which result from the mantle magma underplating below the early subducted oceanic crust. The strike of the dykes was chronically controlled by a sinistral shear mechanism in the area, which might be related to the northward movement of Pacific plate to Asian plate.

       

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