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值得再三思考的唐山地震构造
WORTHWHILE CONSIDERING THE SEISMO-STRUCTURE OF THE TANGSHAN EARTHQUAKE
【摘要】 本文在前人工作的基础上,就现今构造活动与地区性构造的因果关系提出问题,根据唐山地区的勘探成果结合实地调查和形变测量等资料,着重对该区的主体褶皱构造——不对称的开平向斜进行了初步研究,提出发震断层是向斜倒转翼不断遭受剪、压的顺势发展的结果。
【Abstract】 Why a strong earthquake occurs in a specific region? It might be concerned in the specific structures in this area. The preliminary studies are made on the seismo-structure and the related problems in this paper, based on the geological results of the coal field and the geodetic data in the Tangshan epicentral region.It is suggested that the occurrence of the Tangshan earthquake related to both the evolution of the asymmetric Kaiping syncline and its recent activities. The seismic fault is resulted from the evolution of the inverted slope of the syncline that subjected to the continuous pressure and shear. The seismic fault is linked up with the deep fault in the form of arc(listric model).The research on the specific characteristics of the seismo-structure is helpful to deepening the study of seismogeology.
- 【文献出处】 中国地震 ,Earthquake Research In China , 编辑部邮箱 ,1987年S1期
- 【被引频次】14
- 【下载频次】68