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Epicentral Distance Distribution of Seismic Landslides in 5.12 Wenchuan Earthquake

机译:地震山地地震岩土地震地震的震中距离分布

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It has been two years after the Wenchuan earthquake taking place in 12 May, 2008. Researchers are still concerned about what happens to the seismic geohazards. By field investigation and statistical analysis in Chengdu City, the distribution of landslides triggered by the earthquake was analyzed and the correlation analysis between rainfall and seismic landslides were conducted in the extremely earthquake stricken region in Chengdu city and the conclusions are as follows: Geohazards triggered by the Wenchuan earthquake reached the historical peak in numbers. Since then the rainfall has become a major triggering factor of landslide occurrence in the earthquake hit regions and the geohazards will be much more substantial in the future decades. The regional distribution of geohazards follow the 2 linear law with the macro-epicenter, large scale landslides are located within 14.9 km from the macro-epicenter, moderate and small scale landslides within S2.7 km from the macro-epicenter.
机译:在2008年5月12日汶川地震发生后已经有两年了。研究人员仍然关注地震地质曲集型发生的事情。通过现场调查和统计分析在成都市,地震引发的滑坡分布,降雨与地震山体滑坡之间的相关性分析在成都市极其地震灾区进行,结论如下:地质锯齿触发汶川地震达到了数字的历史峰值。从那时起,降雨已经成为地震袭击地区滑坡发生的重大触发因素,而且地质血露植物在未来几十年中将更为重要。地质血清的区域分布遵循2个线性法律,宏观震中,大型山体滑坡距离宏观震中的宏观震级,中等和小型山体积不到14.9公里。

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