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    Volume 47 Issue 8
    Sep.  2022
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    Duan Menglong, Xie Chaoming, Wang Bin, Song Yuhang, Hao Yujie, 2022. Ocean Island Rock Assembly and Its Tectonic Significance in Tangga⁃Sumdo Area, Tibet. Earth Science, 47(8): 2968-2984. doi: 10.3799/dqkx.2021.156
    Citation: Duan Menglong, Xie Chaoming, Wang Bin, Song Yuhang, Hao Yujie, 2022. Ocean Island Rock Assembly and Its Tectonic Significance in Tangga⁃Sumdo Area, Tibet. Earth Science, 47(8): 2968-2984. doi: 10.3799/dqkx.2021.156

    Ocean Island Rock Assembly and Its Tectonic Significance in Tangga⁃Sumdo Area, Tibet

    doi: 10.3799/dqkx.2021.156
    • Received Date: 2021-08-28
    • Publish Date: 2022-09-25
    • The Sumdo (Ultra)high Pressure Metamorphic Zone plays an important role in understanding the evolution of the Paleo Tethys Ocean in Tibet. However, there are few records about the early evolution of the ocean basin on behalf of this zone, which restricts the understanding of the evolution of the Paleo Tethys Ocean. In this paper, we have studied the field geological characteristics, magmatic whole rock geochemistry and zircon U⁃Pb chronology of the ocean island rock assemblages in Tangga area. The field geological characteristics of the ocean island rock assemblages in Tangga area show the typical "double layer structure", with basalt basement in the lower layer, limestone (marble) cover layer and colluvial conglomerate in the upper cover layer, and metamorphic basalt interbedded with marble and tuff in the upper cover layer, which is similar to the "Cape Verde" ocean island. Zircon U⁃Pb geochronology of two basalts and a diabase porphyrite dike is 330 Ma, 310 Ma and 307 Ma, respectively, indicating the least Early Carboniferous to Late Carboniferous. Both basalt and diabase porphyrite have high content of TiO2, P2O5 and (Na2O+K2O). The rare earth elements (REE) and trace element compositions are similar to those of OIB, showing significant enrichment of Nb and Ta, which fall in OIB and intraplate basalt regions in the discriminant diagram. The REE partition curve and the trace element spider diagram are similar to those of OIB, showing obvious Nb and Ta enrichment. The magma source area of basalt and diabase porphyrite may be the spinel⁃garnet peridotite mantle, with a small melting depth, indicating that the overlying lithosphere may be a new⁃born ocean crust with a small thickness. Combined with previous studies, we preliminarily consider that the Sumdo Paleo Tethys Ocean developed an initial ocean basin in the least Early Carboniferous, and it expanded slowly/ultra⁃slowly from the least Early Carboniferous to the Late Carboniferous, forming the ocean island rock assemblages with the characteristics of "Cape Verde" in Tangga area.

       

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