2024年3—6月中国大陆地区M≥4.0地震震源机制解测定  

Determination of focal mechanism solutions of the earthquakes with M≥4.0 occurred in the mainland of China during March to June 2024

作　　者：梁姗姗[1] 邹立晔[1] 刘艳琼 李旭茂 任枭[1] Liang Shanshan;Zou Liye;Liu Yanqiong;Li Xumao;Ren Xiao(China Earthquake Networks Center,Beijing 100045,China)

机构地区：[1]中国地震台网中心,北京100045

出　　处：《地震科学进展》2024年第7期476-482,共7页Progress in Earthquake Sciences

基　　金：中国地震局常规性项目《测震学科技术管理组运维及青年骨干业务交流》资助。

摘　　要：本文利用中国地震台网记录的宽频带波形资料,采用近震全波形反演方法得到2024年3月1日—6月30日发生在中国大陆地区的M≥4.0共59次地震震源机制解。结果显示逆断型18次,走滑型33次,正断型7次,未知型1次。In this paper,the regional full waveform inversion using the broadband waveforms recorded by China Seismic Network were conducted,and the focal mechanism solutions of the 59 earthquakes with M≥4.0 occurred in the mainland of China during March to June 2024 were obtained.The types of these focal mechanism solutions show 18 reverse faulting,33 strike-slip faulting,7 normal faulting and 1 odd earthquakes.

关 键 词：震源机制 震源参数 

分 类 号：P315.33[天文地球—地震学]