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Preliminary Research on the Characteristics of the M_S8.0 Wenchuan Earthquake Hazard
Authors:Li Zhiqiang[]  Yuan Yifan[]  Li Xiaoli[]  Zhang Qin[]  Dai Boyang[]  Ye Youqing[]  Ge Peifeng[] and Zeng Jie[]
Institution:[1]Institute of Geology, China Earthquake Administration, Beijing 100029, China [2]Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, China [3]Earthquake Administration of Hebei Province, Shijiazhuang 050021, China [4]Earthquake Administration of Sichuan Province, Chengdu 610041, China [5]Earthquake Administration of Shimian City, Shimian 625400, Sichuan, China [6]Earthquake Administration of Zigong City, Zigong 643000, Sichuan, China
Abstract:The M_S8.0 Wenchuan earthquake on May 12, 2008 caused heavy casualties and economic loss. According to the field investigations, the characteristics can be described as follows: The meizoseismal region with an intensity of XI shows an obviously zonal distribution and suffered serious destruction from the earthquake, and the destruction perpendicular to the earthquake surface rupture decreased sharply. At the same time, the intensity X and IX regions perpendicular to the rupture are narrow and therefore their coverage area is small. The intensity on both sides of the rupture attenuates rapidly, but intensity VII and the VI regions are wide, the latter covering about 240,000 km~2. In intensity VI region, the damage area perpendicular to the rupture in the southern part is much larger than that of the northern part. Also, much new understanding about destruction types and destructive modes for all kinds of buildings, landforms and terrain is achieved in this paper.
Keywords:Ms8  0 Wenchuan earthquake  Characteristics of earthquake hazard  Intensity distribution
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