Glacial dammed lakes in the Tsangpo River during late Pleistocene, southeastern Tibet
Glacial dammed lakes in the Tsangpo River during late Pleistocene, southeastern Tibet
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DOI：
10.1016/j.quaint.2012.11.004
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发表时间：
2013-06
影响因子：
2.2
通讯作者：
Zhu Song;Wu Zhen-han;Zhao Xitao;Xiao Ke-yan
中科院分区：
文献类型：
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作者：
Zhu Song;Wu Zhen-han;Zhao Xitao;Xiao Ke-yan
利用光激发发光和花粉分析方法对青藏高原的湖泊样品进行了分析，结果表明，青藏高原3个堰塞湖分别发生在末次冰期早期、末次盛冰期晚期和新冰期。
Lacustrine and alluvial terraces and sediments record the extent of at least three stages of late Pleistocene glacially dammed lakes, along the Tsangpo River at the Dazhuka-Yueju gorge, the Zangga-Gyaca gorge and the Grand Bend gorge, in southeastern Tibet. Analysis of lacustrine samples in the Tsangpo River valley by Optically Stimulated Luminescence and pollen analysis showed that the three dammed lakes in the Tsangpo River valley occurred during the early stage of the last glaciation, the later stage of the last glaciation (the Last Glacial Maximum), and the Neoglacial.