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Epicentral Distance Distribution of Seismic Landslides in 5.12 Wenchuan Earthquake

机译:汶川5.12级地震滑坡震中距分布。

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摘要

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:距2008年5月12日汶川地震发生已经两年了。研究人员仍然担心地震地质灾害的后果。通过对成都市的实地调查和统计分析,分析了地震引发的滑坡的分布,并在成都市的特大地震灾区进行了降雨与地震滑坡的相关性分析,结论如下:汶川地震达到了历史最高水平。从那以后,降雨已成为地震灾区滑坡发生的主要触发因素,在未来几十年中,地质灾害将更加严重。地质灾害的区域分布遵循2线性定律,其中宏观上样中心位于距宏观上样中心14.9 km处,中小规模滑坡在宏观上样中心距S2.7 km之内。

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