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《Acta Sedimentologica Sinica》 2002-02
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Pediment near the Western Liupan Mountain and Its Implication on the Neotectonic Uplift

YANG Dong~ (1,2 ) FANG Xiao-min~ (1,3 ) SONG You-gui~ (1,3) Lü Lian-qing~1 LI Ji-jun~1 AN Zhi-sheng~3 1(Key Laboratory of Western China's Environment Systems of Ministry of Education & Department of Geography, Lanzhou University, Lanzho  
The late Cenozoic uplift of the Tibetan Plateau played a great role in the geomorphic and depositional evolution of its adjacent areas. This effect has brought about the Liupan Mountain at the northeastern tectonic margin of the Tibetan Plateau developed with quite different geomorphology in its two sides, resulting in large differences in wind-blown depositional environment between the eastern and western parts of the Chinese Loess Plateau. A well-preserved pediment, covered by 235 m thick loess, was recently found at the western side of the Liupan Mountain, which stands above the highest terrace of the Yellow River in the northeastern Longzhong Basin. The paleomagnetism of the loess section shows that the pediment developed at ~1.8 Ma BP, so did that of the pediments in Lanzhou-Linxia region in the southwestern Longzhong Basin. This implies that the Longzhong Basin to the west of the Liupan Mountain had been subject to long term denudation before ~1.8 Ma BP, and wight have finally developed a joined pediment or so-called Gansu Peneplain covering the whole Longzhong Basin. The large incision of the pediment and start of deposition of loess on the pediment at ~1.8 Ma BP suggest that the Tibetan Plateau and the Liupan Mountain rose strongly at that time, causing not only the end of the pediment but also the subsequent appearance of the Yellow River in the Basin.
【Fund】: 中国科学院引进国外杰出人才计划 (批准号 :人教字 [2 0 0 0 ] 0 0 5号 );; 国家杰出青年科学基金 (批准号 :4992 81 0 );; 国家重点基础研究发展规 划项目 (批准号 :G1 9980 4 0 80 0 )资助。
【CateGory Index】: P542
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