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Analysis of Longitudinal Profiles along the Eastern Margin of the Qinghai-Tibetan Plateau 被引量:3

Analysis of Longitudinal Profiles along the Eastern Margin of the Qinghai-Tibetan Plateau
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摘要 Resulting from the collision of the Eurasian and Indian plates, the Qinghai-Tibetan Plateau is commonly known as the 'roof of the world'. Collectively the Yarlung Tsangpo, Nu, Lancang, Yangtze, Yalong, and Yellow River basins drain the eastern margin of the plateau. In this paper, we utilize Shuttle Radar Topography Mission elevation data to examine morphometric and relief attributes of these basins to reveal insights into tectonic activity and rates of incision. A robust technique using Matlab is proposed to alleviate errors associated with SRTM data in the derivation of river longitudinal profiles. Convex longitudinal profiles are interpreted to be a product of uplift rates that exceed rates of channel incision along the entire margin of the Qinghai-Tibetan Plateau. Highest relief towards the south reflects extensive fluvial incision. High relief is also prominent along major active faults. Erosion patterns are related to distance from knickpoints. Highest rates of erosion and incision are evident towards the south, with decreasing values towards the north, suggesting a link between tectonic activity and erosion. Resulting from the collision of the Eurasian and Indian plates, the Qinghai-Tibetan Plateau is commonly known as the 'roof of the world'. Collectively the Yarlung Tsangpo, Nu, Laneang, Yangtze, Yalong, and Yellow River basins drain the eastern margin of the plateau. In this paper, we utilize Shuttle Radar Topography Mission elevation data to examine morphometric and relief attributes of these basins to reveal insights rates of incision. A robust into tectonic activity and technique using Maflab is proposed to alleviate errors associated with SRTM data in the derivation of river longitudinal profiles. Convex longitudinal profiles are interpreted to be a product of uplift rates that exceed rates of channel incision along the entire margin of the Qinghai- Tibetan Plateau. Highest relief towards the south reflects extensive fluvial incision. High relief is also prominent along major active faults. Erosion patterns are related to distance from knickpoints. Highest rates of erosion and incision are evident towards the south, with decreasing values towards the north, suggesting a link between tectonic activity and erosion.
机构地区 School of Environment
出处 《Journal of Mountain Science》 SCIE CSCD 2013年第4期643-657,共15页 山地科学学报(英文)
基金 Funding was provided by International Science&Technology Cooperation Program of China(Grant Nos.2011DFG93160,2011DFA20820)
关键词 青藏高原东缘 剖面分析 黄河流域 构造活动 印度洋板块 雅鲁藏布江 欧亚板块 高程数据 Longitudinal profile Erosion Relief Tectonics Qinghai-Tibetan Plateau
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  • 1Ahnert F (1984) Local relief and the height limits of mountain ranges. American Journal of Science 284: 1035-1055. DOl: 1O.2475/ajs.284?9?1035.
  • 2An Z, Kutzbach JE, Prell WL, Porter SC (2001) Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times. Nature 411: 62-66. DOl: 10.1038/35075035.
  • 3Beaumont C, Kooi H, Willett S (2000) Coupled tectonic-surface process models with applications to rifted margins and collisional orogens. In: Geomorphology and Global Tectonics, Summerfield, M.A (ed.). Wiley, Chichester. p 29.
  • 4Binnie S, Phillips W, Summerfield M, Fifield L (2007) Tectonic uplift, threshold hillslopes, and denudation rates in a developing mountain range. Geology 35: 743-746. DOl: 10.1130/G23641A?1.
  • 5Bishop P (2007) Long-term landscape evolution: Linking tectonics and surface processes. Earth Surface Processes and Landforms 32: 329-365. DOl: 1O.1002/esp.1493.
  • 6Burbank D, Leland J, Fielding E, Anderson R, Brozovic N (1996) Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas. Nature 379: 505-510. DOl: 1O?1038/379505ao.
  • 7Coleman M, Hodges K (1995) Evidence for Tibetan Plateau uplift before 14 Ma ago from a new minimum age for east?west extension. Nature 374: 45-92. DOl:1O.1038/374049ao.
  • 8Craddock WH, Kirby E, Harkins NH, Zhang H, Shi J (2010) Rapid fluvial incision along the Yellow River during headward basin integration. Nature Geoscience 3: 209-213. DOl: 1O?1038/ngeo777.
  • 9England P, Houseman G (1986) Finite strain calculations of continental deformation II: comparison with the India-Asia collision zone. Journal of Geophysical Research 91: 3664- 3676. DOl: 1O.1029/JB091iB03p03664.
  • 10Finlayson DP, Montgomery DR (2003) Modelling large-scale fluvial erosion in geographical information systems. Geomorphology 53: 147-164. DOl: 1O.1016/S0169-555X(02) 00351-3.

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