中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sediment storage and morphology of the Yalu Tsangpo valley due to uneven uplift of the Himalaya

文献类型:SCI/SSCI论文

作者Wang Z. Y.; Yu, G. A.; Wang, X. Z.; Melching, C. S.; Liu, L.
发表日期2015
关键词Yalu Tsangpo River sediment deposits uneven uplift himalaya wide valley tibetan plateau evolution incision river
英文摘要The fluvial process of the Yalu Tsangpo River occurs concurrently with the uplift of the Qinghai-Tibet Plateau. Therefore, the river exhibits unique features in morphology and sediment deposition. Field investigations were performed from 2009-2011 and the depth of the interface between the sediment deposits and bed rock was detected with an electromagnetic imaging system (EH4) at 29 cross sections. Sediment deposits were sampled along the Yalu Tsangpo valley from Xietongmen to the Yalu Tsangpo Canyon. The results show that a huge amount of sediment has been deposited in four wide valley sections because the uplift rate in these sections was lower than that in the downstream gorge sections over the past million years. About 518 billion m3 of gravel and sand have been stored in the high mountain river valleys, which has changed the V-shaped mountain river valley into a U-shaped wide river valley in the four sections. In the sections with high uplift rates the river bed is incised and has formed gorges and the Yalu Tsangpo Canyon.
出处Science China-Earth Sciences
58
8
1440-1445
收录类别SCI
语种英语
ISSN号1674-7313
源URL[http://ir.igsnrr.ac.cn/handle/311030/38926]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Wang Z. Y.,Yu, G. A.,Wang, X. Z.,et al. Sediment storage and morphology of the Yalu Tsangpo valley due to uneven uplift of the Himalaya. 2015.

入库方式: OAI收割

来源:地理科学与资源研究所

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