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    G. Einsele, S. Dürr, W. Frisch, Liu Guanghua, H. P. Luterbacher, L. Ratschbacher, W. Ricken, J. Weridt, A. Wetzel, Liu Baojun, Yu Guangming, Zheng Haixiang. THE XIGAZE FOREARC BASIN (CRETACEOUS, TIBET): SEDIMENTS AND BASIN EVOLUTION[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(1): 3-31,56.
    Citation: G. Einsele, S. Dürr, W. Frisch, Liu Guanghua, H. P. Luterbacher, L. Ratschbacher, W. Ricken, J. Weridt, A. Wetzel, Liu Baojun, Yu Guangming, Zheng Haixiang. THE XIGAZE FOREARC BASIN (CRETACEOUS, TIBET): SEDIMENTS AND BASIN EVOLUTION[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(1): 3-31,56.
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    THE XIGAZE FOREARC BASIN (CRETACEOUS, TIBET): SEDIMENTS AND BASIN EVOLUTION

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    • The evolution of the Xigaze forearc basin in southern Tibet, as investigated in a 120 km segment along the Indus-Yarlung suture zone, south of the Lhasa block and its plutonic rocks (Gangdise belt) commenced in the mid-Cretaceous on top of trapped oceanic or transitional crust. Relies of the former passive margin sediments, especially shallow-water carbonates, are preserved along the northern edge of the strongly deformed (approximately 65 shortening) and partially eroded basin fill.
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