摘要
本文根据现场考察资料论述了阿尔金山中段南侧地震形变带的基本特征,对地震断层剖面进行了分析,并在此基础上确定了阿尔金山中段南侧大地震的基本参数及其地震成因。
In this paper,the basic feature of seismic deformation belt on the south side of Middle Aerjin has been described according to the observing materials in the field.The basic parameters and seismogenesis of the large earthquakes on the south side of Middle Aerjin have been determined on the bases of seismic fault profile analysis.
作者
贾云鸿
张瑞斌
Jia Yunhong;Zhang Ruibin(Seismological Institute of Lanzhou,SSB;Seismological Bureau of Qinghai Province,Xining)
出处
《内陆地震》
1988年第4期422-427,共6页
Inland Earthquake
关键词
地震
形变
断层
Earthquake
Deformation
Fault
