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《Acta Sedimentologica Sinica》 2002-02
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Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau --I Stratigraphy and Petrology

ZHENG Hong-bo~ 1,2 BUTCHER Katherine~3 POWELL Chris~3 1 ( Laboratory of Marine Geology, Tongji University, Shanghai 200092) 2 (Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054) 3 (Tectonic Special Research Centre, The Un  
Late Ceinozoic forland basin deposits in Yecheng are composed of Miocene mudstone and sandstone (Wuqia Group), Early Pliocene sandstone with minor gritstone (Artux Formation) and Late Pliocene-Early Pleistocene conglomerate (Xiyu Formation). The Miocene strata are dominated by fine-grained clastic material, indicating a distal source and low gradient slope. Palaeocurrent measurements suggested northward direction, indicating that the Kunlun area was at low elevation. Deposition of Artux Formation marked the first appearance of gravel and lithic detritus, indicating the uplift of the Kunlun. Xiyu Formation is characterized by coarse debris flow deposits, marking the strong uplift of the northern part of Tibetan Plateau and unroofing of the Kunlun.
【Fund】: 中国科学院“百人计划” ;; 国家杰出青年基金 (40 0 2 5 1 0 7) ;; 国家重点基础研究发展规划项目 (G2 0 0 0 0 785 0 1 ) ;; 教育部“长江特聘教授”计划资助
【CateGory Index】: P534.63
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