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中国大陆现代构造应力场与强震活动
引用本文:谢富仁,张红艳,崔效锋,杜义.中国大陆现代构造应力场与强震活动[J].国际地震动态,2011(1):4-12.
作者姓名:谢富仁  张红艳  崔效锋  杜义
作者单位:中国地震局地壳应力研究所;
基金项目:中央级公益性科研院所基本科研业务专项(ZDJ2010-07); 国家自然科学基金(40904024)共同资助
摘    要:依据应力性状和力源特征,中国大陆现代构造应力场可划分为四级应力区.它们分别是2个一级应力区、4个二级应力区、5个三级应力区和26个四级应力区.通过分析中国大陆现代构造应力分区与强震活动之问的关系,初步获得以下结论:①构造应力作用强烈和复杂的地区是强震频发的地区;②应力区边界是强震集中发生的地带;③应力方向、应力结构类型...

关 键 词:构造应力场  应力分区  强震活动  动力学

The modern tectonic stress field and strong earthquakes in China
Xie Furen,Zhang Hongyan,Cui Xiaofeng,Du Yi.The modern tectonic stress field and strong earthquakes in China[J].Recent Developments in World Seismology,2011(1):4-12.
Authors:Xie Furen  Zhang Hongyan  Cui Xiaofeng  Du Yi
Affiliation:Xie Furen,Zhang Hongyan,Cui Xiaofeng,Du Yi(Institute of Crustal Dynamics,CEA,Beijing 100085,China)
Abstract:According to the stress state and genetic force character,the modern tectonic stress field of China can be preliminarily divided into 4categories.Within these categories,there are 2first-order districts,4second-order districts,5third-order districts and 26 fourth-order districts.By analyzing those tectonic stress districts and strong earthquakes,the close relation between them is mainly summarized as follows:①Strong earthquakes fre-quently occur in the area with intense and complex tectonic stress action;② Along the boundary of stress districts,especially between the first-or second-order districts controlled by the interaction of tectonic plates,strong earthquakes occur very easily and frequently;③ Strong earthquakes always occur in the zone with a rapid change of stress direction or values;④Strong earthquakes relatively concentrate in the area with local variation of the stress,which situates in the homogeneous background of stress;⑤Stress transformation zone along active faults is more likely to have strong earthquakes.
Keywords:tectonic stress field  stress district  strong earthquakes  dynamics  
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