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	A review of glacial sequences of the Kunlun Pass, northern Tibetan Plateau
	Liu, Gengnian ; Zhang, Xiaoyong ; Cui, Zhijiu ; Wu, Yongqiu ; Ju, Yuanjiang
	2006
关键词	QUATERNARY GLACIATION LATE MIOCENE QINGHAI GEOTRAVERSE EXPANSION PAKISTAN OBLIQUE ORIGIN GROWTH UPLIFT
英文摘要	In the Kunlun Pass area of northern Tibet, glacial landforms and sediments provide evidence for three major Quaternary glaciations. ESR and TL dating suggest that they date to 600-700 ka (Wangkun Glaciation), similar to 260 ka (Yakou Glaciation) and 61-13 ka (Yuzhufeng Glaciation/ the Last Glacial). Each glaciation is less extensive than its predecessor. The Wangkun Glaciation is the largest Quaternary Glaciation. The extent of the glaciers during the Wangkun Glaciation was 3-5 times larger than that of the present glaciers. During the Last Glacial, glaciers advanced several times. The moraines near the modern glaciers are probably the products of Neoglaciation and Little Ice Age. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.; Geography, Physical; Geosciences, Multidisciplinary; SCI(E); CPCI-S(ISTP); 9
语种	英语
DOI标识	10.1016/j.quaint.2006.02.004
内容类型	其他
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/251551]
专题	环境科学与工程学院
推荐引用方式 GB/T 7714	Liu, Gengnian,Zhang, Xiaoyong,Cui, Zhijiu,et al. A review of glacial sequences of the Kunlun Pass, northern Tibetan Plateau. 2006-01-01.

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