Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake-Reference-Cited by-同舟云学术

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Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake

Published:2009-09-27 Issue:10 Volume:2 Page:718-724
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Shen Zheng-Kang,Sun Jianbao,Zhang Peizhen,Wan Yongge,Wang Min,Bürgmann Roland,Zeng Yuehua,Gan Weijun,Liao Hua,Wang Qingliang

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo636.pdf

Reference34 articles.

1. http://www.gov.cn/xxgk/pub/govpublic/mrlm/200805/t20080530_32846.html .

2. Burchfiel, B. C. et al. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People’s Republic of China. GSA Today 18, 4–11 (2008).

3. Xu, X. et al. Coseismic reverse- and oblique-slip surface faulting generated by the 2008 Mw 7.9 Wenchuan earthquake, China. Geology 37, 515–518 (2009).

4. Burchfiel, B. C., Chen, Z., Liu, Y. & Royden, L. H. Tectonics of the Longmen Shan and adjacent regions. Int. Geol. Rev. 37, 661–735 (1995).

5. Jia, D. et al. Longmen Shan fold-thrust belt and its relation to the western Sichuan Basin in central China: New insights from hydrocarbon exploration. AAPG Bull. 90, 1425–1447 (2006).

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