中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sedimentary records of a palaeo-lake in the middle Yarlung Tsangpo: Implications for terrace genesis and outburst flooding

文献类型:期刊论文

作者Chen, F (Chen, Feng)1,3; Feng, JL (Feng, Jin-Liang)1; Hu, HP (Hu, Hai-Ping)1,2
刊名QUATERNARY SCIENCE REVIEWS
出版日期2018-07-15
卷号192期号:0页码:135-148
关键词C-14 YR BP YOUNGER DRYAS TIBETAN-PLATEAU DAMMED LAKE LATE PLEISTOCENE NORTHERN-HEMISPHERE LOESS SEDIMENTATION CHANNELED SCABLANDS SOUTHEASTERN TIBET OCEAN CIRCULATION
ISSN号0277-3791
DOI10.1016/j.quascirev.2018.05.037
英文摘要The middle reaches region of the Yarlung Tsangpo in the southern Tibetan Plateau consist of broad valley reaches, alternating with gorges, which were easily dammed by glaciers and/or glacial moraines during the last glacial period. We investigated three palaeo-lake sedimentary sequences on terraces located in the broad Xigaze valley reach and the Dazhuka-Yueju gorge in the middle reaches of the Yarlung Tsangpo. We found that the altitude of the palaeo-lake was 3811 m above sea level, while its minimum area and volume were similar to 679 km(2) and similar to 22 km(3), respectively. The palaeo-lake was formed during the period from about 30.2 to 32.3 cal. kyr BP, and it failed at about 13.2 cal. kyr BP. The dam was possibly located at the eastern end of the Dazhuka-Yueju gorge and may have been a glacier and/or a moraine during the late part of the last glacial. The failure of the dam and related flooding from the Dazhuka-Yueju gorge probably triggered a chain reaction of dam failures downstream, forming a megaflood. Terrace genesis and valley evolution in the investigated region can be divided into four phases: Phase I (>32.3 cal. kyr BP), river occupation; Phase II (<32.3-13.2 cal. kyr BP), palaeo-lake occupation; Phase III (after 13.2 cal. kyr BP), erosion and aeolian deposition; Phase IV, modern downward incision. (C) 2018 Elsevier Ltd. All rights reserved.
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000438179800010
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://ir.itpcas.ac.cn/handle/131C11/8597]  
专题青藏高原研究所_图书馆
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
2.East China Univ Technol, Sch Earth Sci, Nanchang 330013, Jiangxi, Peoples R China;
3.Shanxi Univ Finance & Econ, Dept Environm Econ, Taiyuan 030006, Shanxi, Peoples R China.
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Chen, F ,Feng, JL ,Hu, HP . Sedimentary records of a palaeo-lake in the middle Yarlung Tsangpo: Implications for terrace genesis and outburst flooding[J]. QUATERNARY SCIENCE REVIEWS,2018,192(0):135-148.
APA Chen, F ,Feng, JL ,&Hu, HP .(2018).Sedimentary records of a palaeo-lake in the middle Yarlung Tsangpo: Implications for terrace genesis and outburst flooding.QUATERNARY SCIENCE REVIEWS,192(0),135-148.
MLA Chen, F ,et al."Sedimentary records of a palaeo-lake in the middle Yarlung Tsangpo: Implications for terrace genesis and outburst flooding".QUATERNARY SCIENCE REVIEWS 192.0(2018):135-148.

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来源:青藏高原研究所

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