汶川大地震中映秀-虹口地区的地表破裂
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摘要
2008年5月12日14:28四川省西部发生Ms8.0级强震,基于对震区第一手的调查资料,在简介映秀-虹口地区地质条件与断裂构造格局的基础上,对该地区地表破裂带及其分布进行分类和描述,并初步探讨地表破裂带与断裂构造的关系及对工程结构的影响。经分析,映秀-北川断裂的逆冲-走滑作用是映秀-虹口地区地表主要破裂带产生的原因,但滑覆体和次级断层的强烈活动也造成了连续的地表破裂,不同地表破裂带对附近工程结构的影响有所区别。
At 14:28,May 12th 2008,a strong earthquake measured Ms 8.0 hit west Sichuan province,PR China.Based on field reconnaissance,a brief introduction to the geology and fault patterns in Yingxiu and Hongkou area was introduced.The surface ruptures,and its relation with fault patterns,which post-quake reconstruction have to face with,were described and discussed.
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