1994年台湾海峡7.3级地震发震断层的地震学证据  

Seismological evidence of seismogenic fault of the M 7.3 Taiwan Strait earthquake

作　　者：彭美凤[1] 周峥嵘[1] 

机构地区：[1]福建省地震局,福建福州350003

出　　处：《华南地震》2000年第3期9-13,共5页South China Journal of Seismology

摘　　要：通过地震学观测资料的分析和研究 ,并综合其他作者的研究成果 ,论证了台湾海峡 1994年 7 3级地震发震断层的主破裂面走向应为北西向 ,地震的发生是由分布于该区域的巴士系构造活动所致。In this paper, the authors proved that the strike of the main fractured surface of the M 7 3 Taiwan Strait earthquake occurred in September 16,1994 must be NW by analyzing the seismic observation data and integrating the research results of other researchers. The authors think that the M 7 3 earfhquake is caused by the activity of the Bashi system tectonic which distributed in this area.

关 键 词：地震断层 断层走向 震源机制 应力场 

分 类 号：P315.2[天文地球—地震学]