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    Volume 46 Issue 2
    Feb.  2021
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    Article Navigation >  Earth Science  > 2021  >  46(2): 381-404
    Fan Jianjun, Li Cai, Niu Yaoling, Xie Chaoming, Wang Ming, 2021. Identification Method and Geological Significance of Intraplate Ocean Island-Seamount Fragments in Orogenic Belt. Earth Science, 46(2): 381-404. doi: 10.3799/dqkx.2020.348
    Citation: Fan Jianjun, Li Cai, Niu Yaoling, Xie Chaoming, Wang Ming, 2021. Identification Method and Geological Significance of Intraplate Ocean Island-Seamount Fragments in Orogenic Belt. Earth Science, 46(2): 381-404. doi: 10.3799/dqkx.2020.348
    shu

    Identification Method and Geological Significance of Intraplate Ocean Island-Seamount Fragments in Orogenic Belt

    doi: 10.3799/dqkx.2020.348
    • 1.

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

    • 2.

      Department of Earth Science, Durham University, Durham DH1 3LE, UK

    • Received Date: 2020-12-16
    • Publish Date: 2021-02-15
      Abstract
    • Fragments of intraplate ocean island-seamount are important parts of "oceanic crust fragments" in the orogenic belt, and these fragments place important constraints on restoring the tectonic evolution of the ancient ocean basin represented by the orogenic belt. However, the identification method and geological significance of the intraplate ocean island-seamount fragments in the orogenic belt are poorly known. Based on the review of the lithological sequence, magmatic rock types, geochemistry, and isotopic characteristics of the intraplate ocean island-seamounts in the modern ocean basin and our research results on several intraplate ocean island-seamount fragments in the Bangongco-Nujiang suture zone in the Tibetan Plateau, in this study it summarizes the identification method, age determination method, and geological significance of the intraplate ocean island-seamount fragments in the orogenic belt. Intraplate ocean island-seamounts record extensive information about the tectonic evolution of the ocean basin, and these are the easiest oceanic geological bodies to preserve during the subduction of the oceanic lithosphere. Therefore, studies on the intraplate ocean island-seamount fragments in the orogenic belt are very important in restoring the tectonic evolution of the ancient ocean basin.

       

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