摘要
在综合分析地裂缝发育特征、地裂缝发育区的地质环境及新构造活动背景基础上,作者认为:山西断陷带的地裂缝是在新构造活动加强的背景下形成的,地下水超采及地层、地貌等非构造环境对地裂缝的发育起着重要的制约作用.
Having comprehensively studied the development characteristics of the earth fissures, its geological environment, and the background of new tectonic activity in Shanxi down faulted basin belt, the authors hold that the earth fissures were formed on condition of intensified tectonic activities. And the over mining of ground water and the factors of non tectonic environments such as landform played an important role for the formation of the earth fissures.
出处
《中国矿业大学学报》
EI
CAS
CSCD
北大核心
1997年第3期74-78,共5页
Journal of China University of Mining & Technology
关键词
山西
断陷带
地裂缝
新构造活动
发育条件
Shanxi down faulted basin belt, earth fissures, tectonic background, developing condition