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    ZHANG Zhan-wu, ZHANG Wen-feng, ZENG Qing-gao, HAN Xiang-tao. Redivision of the stratigraphic sequences and structural patterns of the Upper Triassic Langjiexue Group (Complex) in the Renbu-Qusong stratigraphic subprovince in the eastern part of the Yarlung Zangbo suture zone, Xizang[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(1): 72-80.
    Citation: ZHANG Zhan-wu, ZHANG Wen-feng, ZENG Qing-gao, HAN Xiang-tao. Redivision of the stratigraphic sequences and structural patterns of the Upper Triassic Langjiexue Group (Complex) in the Renbu-Qusong stratigraphic subprovince in the eastern part of the Yarlung Zangbo suture zone, Xizang[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(1): 72-80.
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    Redivision of the stratigraphic sequences and structural patterns of the Upper Triassic Langjiexue Group (Complex) in the Renbu-Qusong stratigraphic subprovince in the eastern part of the Yarlung Zangbo suture zone, Xizang

    • 1. Research Institute of Regional Geology and Mineral Resources, Shaanxi Bureau of Geology and Mineral Resources, Xianyang 712000, Shaanxi, China;

    • 2. Regional Geological Survey Party, Xizang Bureau of Geology and Mineral Resources, Lhasa 850000, Xizang China

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    • Received Date: December 04, 2013
    • Revised Date: December 09, 2013
    • Published Date: March 29, 2014
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      • Abstract
    • Plentiful studies have been conducted in the last decades on the stratigraphic sequences, sedimentary characteristics, deformation and metamorphism, provenance and tectonic settings of the Upper Triassic Langjiexue Group (Complex) in the Renbu-Qusong stratigraphic subprovince in the eastern part of the Yarlung Zangbo suture zone, Xizang. The authors in this study present the redivision of the Langjiexue Group (Complex) on the basis of the existing data on the tectono-lithostratigraphy, palaeontology, deformation and tectonic settings, and contend that the Langjiexue Group (Complex) should be composed, from the base upwards, of the Songre, Jiangxiong and Jiedexiu (Zhangcun) Formations (Complex), and display the structural patterns of a "Ω"-type asymmetrical anticlinorium.
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