Glacial dammed lakes in the Tsangpo River during late Pleistocene, southeastern Tibet

被引：41
|
作者：
Zhu Song [1 ]
Wu Zhen-han [2 ]
Zhao Xi-tao [3 ]
Xiao Ke-yan [1 ]
机构：
[1] Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China
[2] Chinese Acad Geol Sci, Beijing 100037, Peoples R China
[3] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
来源：
QUATERNARY INTERNATIONAL | 2013年 / 298卷
关键词：
D O I：
10.1016/j.quaint.2012.11.004
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
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. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.
引用
收藏
页码：114 / 122
页数：9
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