山西断陷盆地地裂缝特征分析  

Study on the characteristics of ground fissures in Shanxi fault basin

作　　者：陈元明[1] CHEN Yuanming(Shanxi Geological Environment Monitoring Center, Taiyuan,Shanxi 030024, Chin)

机构地区：[1]山西省地质环境监测中心,山西太原030024

出　　处：《中国地质灾害与防治学报》2016年第3期72-80,89,共10页The Chinese Journal of Geological Hazard and Control

摘　　要：山西断陷盆地是我国地裂缝最为发育、破坏性最强、区域特点最典型的地区之一。本文从山西断陷盆地地裂缝的分布规律、发展历史、活动规律、地质构造属性等角度,进行了系统的分析研究,以揭露地裂缝与人口密度、地下水开采、地面沉降、新构造运动、断裂(断层)构造等影响因子之间的关系,在此基础上,总结出山西断陷盆地地裂缝的特征。Shanxi faulted basin in China has become one of the most developed and destructive,the most typical regional features of the area. In this paper,from the distribution law,development history,activity patterns and tectonic attributes of ground fissures,are systemically analyzed and studied,in order to reveal the relationship between the ground fissures and the population density, groundwater exploitation, land subsidence,new tectonic movement,fault structure（ fault） and other factors,on the basis of,summed up the the characteristics of ground fissures in Shanxi fault basin.

关 键 词：山西断陷盆地 地裂缝 集中发育区 地下水超采 新构造运动 第四系断层 

分 类 号：P642.26[天文地球—工程地质学]