Coseismic ruptured creeping Guanxian-Anxian fault during the 2008 Mw 7.9 Wenchuan earthquake (China)
Haibing Li1,2, Xiangli He3,4, Huan Wang4,5, Jialiang Si1,6, Lei Zhang4,7 and Giulio Di Toro8, (1)Key Laboratory of Continental Dynamics, Ministry of Natural Resources, Beijing, China, Beijing, China, (2)State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, (3)Institute of Crustal Dynamics, China Earthquake Administration, Beijing, China, (4)Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Beijing, China, (5)Key Laboratory of Continental Dynamics, Ministry of Natural Resources, Beijing, China, (6)State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, Beijing, China, (7)Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, (8)University of Padova, Department of Geoscience, Padova, Italy
