摘要
对共和主震、强余震震源机制解的P轴方位、仰角、A节面、倾向及M -T的分析 ,认为共和地震是在压力轴方向接近水平的NE向构造应力作用下、沿NW向的断裂带发生的。
P axes,elevation angle,A section,angle of inclination of the mechanism solution of Gonghe main shock and after shocks are analysed in the paper.The result is Gonghe earthquake is a structural earthquake which has obduction and strike-slip movement along the NW fault.
出处
《高原地震》
2001年第4期1-5,共5页
Plateau Earthquake Research
