摘要
本文应用浅层人工地震勘探及地层剖面对比等多种方法对石家庄断裂进行了研究,结果表明该断裂是一条第四纪活动断裂,在市区西部大安舍、留营、玉村、永壁一带通过,呈北8度西展布。并结合地震活动和地壳形变等资料,讨论了该断裂对石家庄市区地壳稳定性的影响,为城市建设规划提供了有力的依据。
This paper made a research on Shijiazhuang fault by varieties of methods such as artificial seismic prospecting and the stratigraphic section contrast etc.. The results indicate that this fault is an active fault at Quaternary Period. It passes through Daanshe, Liuying, Yucun and Yongbi etc., Located at the west of Shijiazhuang City, striking northwest 8°. Moreover, based on the data of seismic activity and crustal deformation etc., the paper discusses the effect of the fault on the crustal st ability of Shijiazhuang City proper. The result has provided a strong foundation for the city's constructive programme.
出处
《华北地震科学》
北大核心
1991年第4期12-23,共12页
North China Earthquake Sciences
