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LIANG Yin-ping, ZHANG Ke-xin, SONG Bo-wen, WANG Guo-can, XU Ya-dong, CHEN Rui-ming, CHNE Fen-ning, LUO Man-sheng. 2013: Paleocene tectonic lithofacies paleogeography of the Tibetan Plateau. Geological Bulletin of China, 32(1): 67-74. DOI: 10.12097/gbc.20130106
Citation: LIANG Yin-ping, ZHANG Ke-xin, SONG Bo-wen, WANG Guo-can, XU Ya-dong, CHEN Rui-ming, CHNE Fen-ning, LUO Man-sheng. 2013: Paleocene tectonic lithofacies paleogeography of the Tibetan Plateau. Geological Bulletin of China, 32(1): 67-74. DOI: 10.12097/gbc.20130106
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Paleocene tectonic lithofacies paleogeography of the Tibetan Plateau

  • Geological publishing House,Beijing 100083;2. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, Hubei, China;3. Faculty of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, Hubei, China;4. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, Hubei, China;5. Institute of Geology and Mineral Resources, China Geological Survey, Xi'an 710054, Shaanxi, China

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  • Based on an integrated study of the geological maps and previous achievements, the authors analyzed the attributes, tectonic settings and lithofacies-stratigraphic sequences of the remnant basins in the Tibetan plateau. In Paleocene, the Tibetan Plateau was characterized by the erosional areas in western Kunlun, Altun, Qilian, western Qinling, Songpan-Garze and Gangdise, the Alxa and Indian ancient lands and the depressed basins (lakes and pluvial plains) in Xining-Lanzhou, Chengdu and Baingoin. There existed Neo-Tethyan remnant sea in western and southern Tibetan Plateau. It is held that the paleogeography of the Neo-Tethyan remnant sea was a remnant oceanic basin to the west of the Saga area and a foreland basin to the east of Saga during the Paleocene. The authors argue that the closure of the Neo-Tethys progressed from east to west.
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