四川甘孜泸定M5.6地震机理分析  

Analysis of M5.6 Earthquake Mechanism in Luding,Ganzi,Sichuan

作　　者：代青沁 Dai Qing-qin(Dalian Earthquake Monitoring Center Station in Liaoning Province,Dalian,Liaoning 116001)

机构地区：[1]辽宁省大连地震监测中心站,辽宁大连116001

出　　处：《农业灾害研究》2023年第11期326-328,共3页Journal of Agricultural Catastrophology

摘　　要：四川甘孜泸定在2023年1月26日发生了M5.6地震,中国地震台网中心发布的信息显示该地震达到了11 km震源深度。此次地震属于正断型,鲜水河主干断裂西侧为震中。为了更为深入地了解此次地震,深入分析四川甘孜泸定M5.6地震机理,为相关工作人员开展地震预防工作提供参考。The M5.6 earthquake occurred in Luding,Ganzi,Sichuan on January 26,2023.According to the information released by the China Earthquake Networks Center Center,the earthquake reached a focal depth of 11km.This earthquake belongs to the normal fault type,with the epicenter located to the west of the Xianshui River main fault.In order to gain a deeper understanding of this earthquake,this article will conduct an in-depth analysis of the M5.6 earthquake mechanism in Luding,Ganzi,Sichuan,hoping to provide reference for relevant personnel to carry out earthquake prevention work.

关 键 词：地震机理 震源机制 泸定M5.6地震 

分 类 号：TU352.11[建筑科学—结构工程]