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    中国百强科技报刊

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    Volume 46 Issue 1
    Jan.  2021
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    Article Navigation >  Earth Science  > 2021  >  46(1): 87-100
    Lian Chenqin, Li Gangzhu, Yu Yang, Yao Fojun, Zhang Siyuan, Wang Pijun, Cui Shunyao, 2021. LA-ICP-MS Zircon U-Pb Age and Whole-Rock Geochemistry of the Triassic Intrusive Rocks in the Solon Obo Area, Inner Mongolia and Its Geological Significance. Earth Science, 46(1): 87-100. doi: 10.3799/dqkx.2019.014
    Citation: Lian Chenqin, Li Gangzhu, Yu Yang, Yao Fojun, Zhang Siyuan, Wang Pijun, Cui Shunyao, 2021. LA-ICP-MS Zircon U-Pb Age and Whole-Rock Geochemistry of the Triassic Intrusive Rocks in the Solon Obo Area, Inner Mongolia and Its Geological Significance. Earth Science, 46(1): 87-100. doi: 10.3799/dqkx.2019.014
    shu

    LA-ICP-MS Zircon U-Pb Age and Whole-Rock Geochemistry of the Triassic Intrusive Rocks in the Solon Obo Area, Inner Mongolia and Its Geological Significance

    doi: 10.3799/dqkx.2019.014
    • 1.

      School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      Hohhot Natural Resources Comprehensive Survey Center, China Geological Survey, Huhhot 010010, China

    • 3.

      Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 4.

      Institution of Geological Survey, China University of Geosciences, Wuhan 430074, China

    • Received Date: 2019-01-28
    • Publish Date: 2021-01-15
      Abstract
    • The Early Mesozoic Zhuendaoouenhuer intrusion is located in Solon Obo area,Inner Mongolia. It mainly consists of hornblende monzonite and monzodiorite.LA-ICP-MS zircon U-Pb dating yields the Early-Triassic age of 248±1 Ma for the hornblende monzonite. Both the hornblende monzonite and monzodiorite are rich in silica (SiO2=51.82%-60.17%),MgO(Mg#=53.17-59.03),alkali (K2O+Na2O=7.36%-9.83%) and Na(K2O/Na2O=0.25-0.53),suggesting a typical alkaline series with the metaluminous feature (A/CNK=0.53-0.75).The rocks are poor in rare earth elements(ΣREE=117.52×10-6-160.89×10-6),enriched in LREE[(La/Yb)N=9.57-15.42] and LILEs (Ba、Sr),and depleted in HFSE,especially Nb,Ta,Ti,Y,and insignificant Eu anomalies(δEu=0.76-1.00),and had high Sr,low Y,high Sr/Y ratio,suggesting geochemical characteristics of high-Mg adakite diorite. The combination of geological setting and geochemical characteristics of the Zhuendaoouenhuer high-Mg adakitic rocks were most probably derived from partial melting of the remnant Paleo-Asian oceanicsubducted slabs and subsequently hybridized by mantle peridotite. The formation of the Zhuendaoouenhueradakitic intrusive rocks is related to the extension of the collision between the North China plate and the Siberian plate. These new age and rock geochemical data indicate that the ancient Asian Ocean closed earlier than 248 Ma.

       

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