龙门山晚新生代地表剥蚀量的定量估算

王岩; 刘少峰; 付碧宏; 邢树文

doi:10.3799/dqkx.2015.080

Volume 40 Issue 6

Jun. 2015

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Article Navigation > Earth Science > 2015 > 40(6): 953-964, 1060

Wang Yan, Liu Shaofeng, Fu Bihong, Xing Shuwen, 2015. Quantitative Estimation of Surface Denudation in Longmen Shan during Late Cenozoic. Earth Science, 40(6): 953-964, 1060. doi: 10.3799/dqkx.2015.080

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Wang Yan, Liu Shaofeng, Fu Bihong, Xing Shuwen, 2015. Quantitative Estimation of Surface Denudation in Longmen Shan during Late Cenozoic. Earth Science, 40(6): 953-964, 1060. doi: 10.3799/dqkx.2015.080

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Quantitative Estimation of Surface Denudation in Longmen Shan during Late Cenozoic

doi: 10.3799/dqkx.2015.080

1.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, MLR Key Laboratory of Metallogeny and Mineral Assessment, Beijing 100037, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
3.
Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, Beijing 100094, China

Received Date: 2014-11-23
Publish Date: 2015-06-15

Abstract

Abstract

Longmen Shan located at the eastern margin of Tibetan Plateau represents the steepest gradient of the Tibetan Plateau edges. To assess the large-scale denudation volume in Longmen Shan, Late Cenozoic, surface denudation is quantitatively calculated along several large drainage basins such as Qingyijiang, Minjiang, Tuojiang, and Fujiang rivers by using digital elevation models (DEM) data, and residual surface method with paleo-residual surface DEM minus modern surface topography in this study. It is found that the Late Cenozoic denudation volume of upper reaches in Longmen Shan drainage basin is between 80 500 and 92 800 km³. Minjiang River has the largest contribution ratio to denudation in Longmen Shan (33.9%-37.1%), followed by Fujiang (33.6%-38.4%) and Qingyijiang Rivers (24.1%-31.9%), and Tuojiang River has minimum contribution (0.4%-0.6%). A rapid erosional removal from the Longmen Shan by repeated great seismic events like the Wenchuan earthquake on May 12th, 2008, may be a main reason of the surface erosion in Late Cenozoic Longmen Shan along the eastern margin of Tibetan Plateau.
- Longmen Shan,
- Late Cenozoic,
- denudation,
- quantitative analysis,
- residual surface,
- tectonics

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Quantitative Estimation of Surface Denudation in Longmen Shan during Late Cenozoic

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