摘要
本文论述了赤金堡—金塔断裂带的基本特征。第四纪以来的活动性及其与地震的关系等问题。提出,该断裂带是阿尔金山断裂带的东延部分。
This article has discussed the basic features of the Chijinpu-Jinta fault zone.It is indicated that the Chijinpu-Jinta fault zone started from Daba runs along the southern margent of the Jinta basin in a direction of about E-W.It has a total length over 200km,and consists of four en echelon fault zones.Finally,the author pointed out that the Chijinpu-Jinta fault zone is probably the eastern continuation of the Aerjinshan fault zone.
作者
王多杰
Wang Duojie(Seismological Institute of Lanzhou,State Seismological Bureau,China)
出处
《内陆地震》
1988年第2期142-146,共5页
Inland Earthquake
