鄂西秭归5．1级地震构造条件研究  

A STUDY ON SEISMOTECTONIC ENVIROMENT OF THE ZIGUI EARTHQUAKE WITH M = 5.1 IN WESTERN HUBEI PROVINCE

作　　者：韩晓光[1] 刘忠书[1] 李安然 

机构地区：[1]国家地震局地震研究所

出　　处：《地震研究》1994年第1期61-66,共6页Journal of Seismological Research

摘　　要：在对震中区及其外缘区域考察和有关资料分析基础上，本文对１９７９年鄂西秭归龙会观５．１级地震的发震构造进行了探讨。结论认为：通过震中区的一组北东向断裂为龙会观地震的主要发震构造。In this paper, based on investigating the tectonic enviroment in and around the epicentral region and analysing relative data authors study seismogenic structure of the 1979 Zigui earthquake with M= 5.1 in western Hubei province and think that a group of NE faults through the epicentral region are the main seismogenic structure of the event.

关 键 词：区域构造 构造条件 地震 震级 

分 类 号：P315.2[天文地球—地震学]