中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Preservation of a large-scale bedrock peneplain suggests long-term landscape stability in southern Tibet

文献类型:期刊论文

作者Strobl, M.1; Hetzel, R.1; Ding, L.2,3; Zhang, L.2,3; Hampel, A.4
刊名ZEITSCHRIFT FUR GEOMORPHOLOGIE
出版日期2010-12-01
卷号54期号:4页码:453-466
关键词Tibetan Plateau peneplain landscape evolution
ISSN号0372-8854
DOI10.1127/0372-8854/2010/0054-0023
文献子类Article
英文摘要Extensive areas with low relief constitute the dominant geomorphic element of the central and southern Tibetan Plateau and were previously interpreted to result from the progressive filling of internally drained basins with sediments derived from adjacent mountain ranges that have been largely eroded. Here we document a completely different low-relief landscape in the Lhasa block of southern Tibet (similar to 31 degrees N, similar to 90 degrees E), where a large-scale peneplain carved into Cretaceous granitoids is well preserved north of lake Nam. Around the town of Bangoin this bedrock peneplain occurs at a constant elevation of similar to 5,300 m in a region not affected by active faulting. The main planation surface has been incised by streams resulting in a local relief of up to 700 m. Progressive fluvial incision generated additional flat bedrock surfaces of limited extent that occur at lower elevations than the peneplain. Local hillslope gradients in the peneplain region increase with decreasing elevation, which is in marked contrast to the morphology of nearby mountain ranges that are uplifted in the footwall blocks of active normal faults. The subsiding hanging walls of these normal faults provide the necessary accomodation space for the sediment produced by erosion of the peneplain region. These relations demonstrate that the bedrock peneplain is the most stable geomorphic element present in southern Tibet.
WOS关键词LHASA BLOCK ; PLATEAU ; MIOCENE ; GEOTRAVERSE ; ELEVATION ; MAGMATISM ; HISTORY ; BASINS ; GOLMUD ; UPLIFT
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000285173700003
出版者GEBRUDER BORNTRAEGER
资助机构German Research Foundation (DFG)(HE 1704/8-1 ; German Research Foundation (DFG)(HE 1704/8-1 ; 1372) ; 1372) ; German Research Foundation (DFG)(HE 1704/8-1 ; German Research Foundation (DFG)(HE 1704/8-1 ; 1372) ; 1372) ; German Research Foundation (DFG)(HE 1704/8-1 ; German Research Foundation (DFG)(HE 1704/8-1 ; 1372) ; 1372) ; German Research Foundation (DFG)(HE 1704/8-1 ; German Research Foundation (DFG)(HE 1704/8-1 ; 1372) ; 1372)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72389]  
专题中国科学院地质与地球物理研究所
通讯作者Strobl, M.
作者单位1.Univ Munster, Inst Geol & Palaontol, D-48149 Munster, Germany
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
4.Leibniz Univ Hannover, Inst Geol, D-30167 Hannover, Germany
推荐引用方式
GB/T 7714
Strobl, M.,Hetzel, R.,Ding, L.,et al. Preservation of a large-scale bedrock peneplain suggests long-term landscape stability in southern Tibet[J]. ZEITSCHRIFT FUR GEOMORPHOLOGIE,2010,54(4):453-466.
APA Strobl, M.,Hetzel, R.,Ding, L.,Zhang, L.,&Hampel, A..(2010).Preservation of a large-scale bedrock peneplain suggests long-term landscape stability in southern Tibet.ZEITSCHRIFT FUR GEOMORPHOLOGIE,54(4),453-466.
MLA Strobl, M.,et al."Preservation of a large-scale bedrock peneplain suggests long-term landscape stability in southern Tibet".ZEITSCHRIFT FUR GEOMORPHOLOGIE 54.4(2010):453-466.

入库方式: OAI收割

来源:地质与地球物理研究所

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