Interpreting the Coseismic Uplift and Subsidence of the Longmen Shan Foreland Basin System during the Wenchuan Earthquake by a Elastic Flexural Model
Author:
Affiliation:
1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (CDUT); Chengdu 610059 China
2. Sichuan Earthquake Administration; Chengdu 610041 China
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/1755-6724.12690/fullpdf
Reference66 articles.
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2. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People's Republic of China;Burchfiel;GSA Today,2008
3. Tectonics of the Longmen Shan and adjacent regions, central China;Burchfiel;International Geology Review,1995
4. Causes of spatially variable tectonic subsidence in the Miocene Bermejo Foreland Basin, Argentina;Cardozo;Basin Research,2001
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1. Differential strain transfer, Longmen Shan thrust belt, eastern Tibetan Plateau margin: Implications for seismic hazards;Journal of Asian Earth Sciences;2019-01
2. Crustal Uplift in the Longmen Shan Mountains Revealed by Isostatic Gravity Anomalies along the Eastern Margin of the Tibetan Plateau;Acta Geologica Sinica - English Edition;2018-02
3. Coupling between the dynamic processes at depth and geologic processes on the surface of the Longmenshan thrust belt;CHINESE J GEOPHYS-CH;2017
4. The Coupling Relationship between the Uplift of Longmen Shan and the Subsidence of Foreland Basin, Sichuan, China;Acta Geologica Sinica - English Edition;2017-04
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