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    Liu Baojun, Yu Guangming, Xu Qiang, G. Einsele, W. Frisch, Liu Guanghua, J. Wendt, A. Wetzel, L. Ratschbacher, H. P. Luterbacher. FORMATION AND EVOLUTION OF THE MESOZOIC AND CENOZOIC DEEP-WATER SEDIMENTARY BASINS ALONG THE YARLUNG ZANGBO RIVER(Ⅰ): SEDIMENTARY CHARACTERISTICS AND EVOLUTION OF THE HIMAIAYAN OROGENIC ZONE[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(1): 32-49.
    Citation: Liu Baojun, Yu Guangming, Xu Qiang, G. Einsele, W. Frisch, Liu Guanghua, J. Wendt, A. Wetzel, L. Ratschbacher, H. P. Luterbacher. FORMATION AND EVOLUTION OF THE MESOZOIC AND CENOZOIC DEEP-WATER SEDIMENTARY BASINS ALONG THE YARLUNG ZANGBO RIVER(Ⅰ): SEDIMENTARY CHARACTERISTICS AND EVOLUTION OF THE HIMAIAYAN OROGENIC ZONE[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(1): 32-49.
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    FORMATION AND EVOLUTION OF THE MESOZOIC AND CENOZOIC DEEP-WATER SEDIMENTARY BASINS ALONG THE YARLUNG ZANGBO RIVER(Ⅰ): SEDIMENTARY CHARACTERISTICS AND EVOLUTION OF THE HIMAIAYAN OROGENIC ZONE

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    • There are similar sedimentary characteristics in the areas from the northern slope of the Himalayas to Lhasa and to Xainza in the Palaeozoic. The Carboniferous-Permian distinctive Gondwana glaciomarine sediments and cold-water faunas indicate that the study area was still then a part of the Indian plate.
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