Analysis of longitudinal profiles along the eastern margin of the Qinghai-Tibetan Plateau

被引:20
作者
Aiken, Simon J. [1 ]
Brierley, Gary J. [1 ]
机构
[1] Univ Auckland, Sch Environm, Auckland 1010, New Zealand
基金
对外科技合作项目(国际科技项目);
关键词
Longitudinal profile; Erosion; Relief; Tectonics; Qinghai-Tibetan Plateau; STREAM POWER; THRESHOLD HILLSLOPES; SEDIMENT DISCHARGE; DENUDATION RATES; FLUVIAL INCISION; BEDROCK INCISION; TECTONIC UPLIFT; QILIAN-SHAN; RIVER; MANTLE;
D O I
10.1007/s11629-013-2814-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
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.
引用
收藏
页码:643 / 657
页数:15
相关论文
共 51 条
[1]   LOCAL RELIEF AND THE HEIGHT LIMITS OF MOUNTAIN RANGES [J].
AHNERT, F .
AMERICAN JOURNAL OF SCIENCE, 1984, 284 (09) :1035-1055
[2]   Evolution of Asian monsoons and phased uplift of the Himalayan Tibetan plateau since Late Miocene times [J].
An, ZS ;
Kutzbach, JE ;
Prell, WL ;
Porter, SC .
NATURE, 2001, 411 (6833) :62-66
[3]  
[Anonymous], 1957, U.S. Geological Survey Professional Paper 294-B, DOI DOI 10.3133/PP294B
[4]  
Beaumont C., 2000, Geomorphology and Global Tectonics, P29
[5]   Tectonic uplift, threshold hillslopes, and denudation rates in a developing mountain range [J].
Binnie, Steven A. ;
Phillips, William M. ;
Summerfield, Michael A. ;
Fifield, L. Keith .
GEOLOGY, 2007, 35 (08) :743-746
[6]   Long-term landscape evolution: linking tectonics and surface processes [J].
Bishop, Paul .
EARTH SURFACE PROCESSES AND LANDFORMS, 2007, 32 (03) :329-365
[7]   Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas [J].
Burbank, DW ;
Leland, J ;
Fielding, E ;
Anderson, RS ;
Brozovic, N ;
Reid, MR ;
Duncan, C .
NATURE, 1996, 379 (6565) :505-510
[8]   EVIDENCE FOR TIBETAN PLATEAU UPLIFT BEFORE 14-MYR AGO FROM A NEW MINIMUM AGE FOR EAST-WEST EXTENSION [J].
COLEMAN, M ;
HODGES, K .
NATURE, 1995, 374 (6517) :49-52
[9]   Rapid fluvial incision along the Yellow River during headward basin integration [J].
Craddock, William H. ;
Kirby, Eric ;
Harkins, Nathan W. ;
Zhang, Huiping ;
Shi, Xuhua ;
Liu, Jianhui .
NATURE GEOSCIENCE, 2010, 3 (03) :209-213
[10]   FINITE STRAIN CALCULATIONS OF CONTINENTAL DEFORMATION .2. COMPARISON WITH THE INDIA-ASIA COLLISION ZONE [J].
ENGLAND, P ;
HOUSEMAN, G .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1986, 91 (B3) :3664-3676