摘要
以唐曹铁路地震安全性评价项目探测断裂为例,采用浅层地震勘探、小折射和钻探等综合地球物理方法,查明宁河—昌黎断裂的展布情况,并结合钻孔资料判定断层的活动时代。研究结果表明,宁河—昌黎断裂呈NEE向展布,由南、中、北3段组成,南北两段以正断为主,中段为走滑性质,为早—中更新世断裂。补充和丰富了该地区的地球物理勘探资料,为该地区的地震安全性评价,国土资源规划等提供基础资料。
In the seismic safety evaluation of Tang-cao railway project,we use synthesis geophysical methods including shallow seismic exploration,refraction,drilling to find out the distribution and activity time of the Ninghe-changli fault conbining with drilling data.The results show that the Ninghe-changli fault is an early-middle Pleistocene fault which extends in dirction of NEE and cosists of 3segment:south segment,middle segment and north segment,the south segment and north segment are mainly normal type while the the middle is strike-slip type.The study supplements and enrichs the geophysical prospecting data of the region and provides basic data for the seismic safety evaluation,land planning,et al.
出处
《华北地震科学》
2016年第1期21-29,共9页
North China Earthquake Sciences
基金
河北省地震科技星火计划项目(DZ20140714052)