摘要
本溪市位于辽东半岛北端。处于阴山东西向复杂构造带的东延与新华夏系第二巨型隆起带的交接部位,属太子河凹陷带,这两种构造体系在区内复合、交接,奠定了本溪地区的基本构造轮廓,本文主要总结了本溪市区及二县地区的地质构造条件和地震活动概况。
In Benxi northern liaodong peninsula. In east extension of yinshan east-west complex tectonic belt and new cathaysian second giant uplift belt of the transition area, with a taizi river sag, these two kinds of composite structural system within the areas, transferring, laid the basic construction of benxi area outline, this paper mainly summarizes the benxi city and county area the general situation of the geological structure conditions and seismic activity.
出处
《防灾减灾学报》
2015年第2期51-57,共7页
Journal of Disaster Prevention And Reduction
关键词
地震
地质
背景
earthquake
geological
background
