Complex Seismic Focus Structure and Earthquake-Triggered Landslide Distribution:Analysis of the 2014 Ludian M_w6.1 Earthquake in Yunnan

查看全文 作　　者：CHEN [1]Xiaoli;LIU [2]Chunguo 机构地区：[1]Key Lab of Active Tectonics and Volcano,Institute of Geology,China Earthquake Administration,Beijing 100029,China;[2]China Earthquake Networks Center,Beijing 100045,China 出　　处：《Acta Geologica Sinica(English Edition)》索引2017年第91卷第2期,共2页 基　　金：supported by the National Natural Science Foundation of China(grant No.41572194);the Institute of Geology,China Earthquake Administration(grant No.IGCEA1604);the National Key Basic Research Program of China(grant No.2013CB733205) 摘　　要：Objective The 2014 Ludian M_w6.1 earthquake in Yunnan occurred in a mountainous area with complex tectonics and topography,which caused serious damage as well as co-seismic landslides of an unusual large scale.Because the suspected seismogenic faults on the surface,distribution of aftershocks and focal mechanism 关 键 词：Complex Seismic Focus Structure and Earthquake-Triggered Landslide Distribution:Analysis of the 2014 Ludian M_w6.1 Earthquake in Yunnan