摘要
本文利用二十多年来大面积水准及跨断层短水准测量资料,首次系统讨论了山西断陷带的总体垂直形变特征及其与地震之间的关系。认为在活动构造带内,垂直差异运动过程中状态的变化是地震孕育,发生的重要因素。
This paper takes advantage of large-area leveling data and short level data obtained across fault in recent 20 years or more, and discusses the characteristics of vertical deformation in Shanxi fault zone as a whole,as well as their relations with earthquakes. It is concluded that the change of the states in the process of vertical motion in active tectonic belts is a important factor of yielding earthquakes.
出处
《地壳形变与地震》
CSCD
1991年第3期63-68,共6页
Crustal Deformation and Earthquake
