论文部分内容阅读
本文根据对大灰厂、牛口峪两台地质地貌条件和断层破碎带的物质组分和形变资料变化过程的分析,讨论了在唐山地震前后两次形变异常的特征和形成原因,认为主要是断层破碎带中含水量变化所致。
Based on the analysis of two geological and geomorphological conditions and the process of material deformation and deformation of the fault crushed zone in Dachaiyou and NiuKouYu, this paper discusses the characteristics and causes of the two deformation anomalies before and after the Tangshan earthquake, and considers that they are mainly Fault rupture zone caused by changes in water content.