摘要
在野外地质调查的基础上,通过研究秦皇岛市F1、F2、F3断裂断层泥中石英颗粒表面的SEM特征,认为F1断裂最末一次活动时间在早更新世至中更新世;F2断裂最末一次活动时间在晚更新世中晚期;F3断裂最末一次活动时间在晚更新世末或全新世初。
On the basis of field geological investigation, through studing the SEM characteristics of quarts grain from pug in faults F1,F2,F3 in Qinhuangdao city, it is considered that the latest active time of F1 fault was in early-mid Pleistocene,the latest active time of F2 fault was in middle-late period of late Pleistocene,and the latest active time of F3 fault was in the end of late Pleistocene or early Holocene.
出处
《内陆地震》
1996年第2期134-138,共5页
Inland Earthquake
关键词
断层泥
断层活动性
断裂
地震地质
Pug Fault activity Scanning electron micrography