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摘要:
Objective Geomorphology has played a central role in the study of active orogenic belts.Extensive tectonic deformation associated with the collision of the Indian and Eurasian plates has occurred in the southeastern margin of the Tibetan Plateau, particularly along the Lancang River Orogenic Belt (LROB) and the Lancang River Fault.Therefore, the landscape evolution of the LROB has significant implications for understanding the tectonic process of intracontinental mountain building and plateau growth.In this study, we used digital elevation models (DEMs) to extract longitudinal profile information on the fluvial systems of the central segment of the LROB.The paleolongitudinal profile developed on the low-relief landscape was reconstructed and the data were used to estimate the amount of surface uplift in the central segment of the LROB.The main purpose of this study was to detect the channel response to tectonic deformation in the southeastern Tibetan Plateau.
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篇名 Transient Fluvial Incision in the Central Segment of the Lancang River Orogenic Belt, Yunnan Province, SW China
来源期刊 地质学报(英文版) 学科
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年,卷(期) 2020,(5) 所属期刊栏目 RESEARCH ADVANCES
研究方向 页码范围 1728-1730
页数 3页 分类号
字数 语种 英文
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序号 姓名 单位 发文数 被引次数 H指数 G指数
1 SHI Xiaohui 1 0 0.0 0.0
2 LI Tingting 1 0 0.0 0.0
3 PEI Lixin 1 0 0.0 0.0
4 WANG Qingtao 1 0 0.0 0.0
5 HUI Bo 1 0 0.0 0.0
6 CHENG Chao 1 0 0.0 0.0
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地质学报(英文版)
双月刊
1000-9515
11-2001/P
16开
北京复外百万庄26号
1922
eng
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