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    Volume 44 Issue 10
    Nov.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(10): 3454-3468
    Cheng Yang, Xiao Qinghui, Li Tingdong, Guo Lingjun, Li Yan, Fan Yuxu, Pang Jinli, 2019. Magmatism and Tectonic Background of Early Permian Intra-Oceanic Arc in Diyanmiao Subduction Accretion Complex Belt in Eastern Margin of Central Asian Orogenic Belt. Earth Science, 44(10): 3454-3468. doi: 10.3799/dqkx.2019.085
    Citation: Cheng Yang, Xiao Qinghui, Li Tingdong, Guo Lingjun, Li Yan, Fan Yuxu, Pang Jinli, 2019. Magmatism and Tectonic Background of Early Permian Intra-Oceanic Arc in Diyanmiao Subduction Accretion Complex Belt in Eastern Margin of Central Asian Orogenic Belt. Earth Science, 44(10): 3454-3468. doi: 10.3799/dqkx.2019.085
    shu

    Magmatism and Tectonic Background of Early Permian Intra-Oceanic Arc in Diyanmiao Subduction Accretion Complex Belt in Eastern Margin of Central Asian Orogenic Belt

    doi: 10.3799/dqkx.2019.085
    • 1.

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

    • 2.

      Institute of Mineral Research, China Metallurgical Geology Bureau, Beijing 101300, China

    • 3.

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

    • Received Date: 2019-04-18
    • Publish Date: 2019-11-11
      Abstract
    • The discovery of petrological evidence for the ocean-continent conversion (intra-oceanic arc) makes it possible to identify, reconstruct and study the ocean-continent conversion. In this paper, the ophiolite in the Diyanmiao subduction accretion complex belt in the eastern margin of the Central Asian orogenic belt was studied in terms of petrogeochemistry, Sr-Nd isotope and zircon U-Pb geochronology, and a set of igneous assemblages in the intra-oceanic arc were identified. The zircon U-Pb concordant age of MORB-like basalt is 286.1±6.1 Ma, representing the period of initial subduction in the ocean. The zircon U-Pb concordant age of HMA is 283.7±4.7 Ma, which represents the age of magmatism when subduction deepened after the first magmatic action. The zircon U-Pb concordant age of IAT is 241±5 Ma, indicating that the paleo-Asian Ocean developed towards continental transition of normal island arc magmatism in the Early Triassic. The sequence of rock assemblages from MORB-like to HMA to IAT represents the progressive evolution of intra-oceanic subduction from shallow to deep and the gradual evolution of ocean basin to the island arc of the continental marginal.

       

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