摘要
采用大地震诱发崩塌滑坡特点与地面破坏程度相结合,以及极震区几何中心方法,定性判定了汶川大地震的宏观震中位置。判定结果是汶川大地震应该有2个宏观震中,一是映秀镇牛圈沟为映秀极震区宏观震中,坐标位置:31.045 6°N,103.455 6°E;二是北川老县城为北川极震区宏观震中,坐标位置:31.863 7°N,104.361 0°E。两种判定方法相比,前者更符合山区特殊地质地貌环境下的地震破坏规律。
The macro-epicenter of Wenchuan earthquake is qualitatively determined by the method of combining the characteristics of earthquake-induced landslides and collapses with ground destructiveness,and the geometric center of the extreme seismic zone.Results show that Wenchuan earthquake should have two macro-epicenters.One is Niujuan canyon in Yingxiu extreme seismic region with coordinates as 31.045 6°N,103.455 6°E,and the other is Beichuan county in Beichuan extreme seismic zone with coordinates as 31.863 7°N,104.361 0°E.Two judging methods are compared,and the former is proved to be more in line with the law of earthquake destruction in the mountainous areas with special geological and geomorphological environment.
出处
《灾害学》
CSCD
北大核心
2013年第1期1-5,共5页
Journal of Catastrophology
基金
"十二五"科技支撑计划项目(2011BAK12B01)
国家重点基础研究("九七三")项目(2010CB731504)
关键词
汶川8级地震
宏观震中
震中判定
Wenchuan M8.0 earthquake
macro-epicenter
epicenter determination