摘要
在野外地质地貌调查的基础上 ,研究了太行山东南麓主要断裂的第四纪水平运动特征。通过调查流经大断裂两侧河流所产生的多种地质地貌变形 ,总结了断裂第四纪水平活动的地质地貌特征 。
The characteristics of horizontal movements in quaternary period of south eastern Taihang Mountain faults are studied on the basis of geological and geomorphological field investigations The characteristics of horizontal movements in quaternary period of south eastern Taihang Mountain faults are summarized and the faults slipping rate is given through investigations of various geological and geomorphological distortions produced by rivers on the two sides of the large faults
出处
《山西地震》
2000年第2期13-17,共5页
Earthquake Research in Shanxi
关键词
断裂带
第四纪
地质演化
地貌特征
太行山
Fracture zone
Quaternary
Geologica evolution
South-eastern of Taihang Mountain
