摘要
通过对浑河断裂(沈阳～抚顺段)不同段落上的地貌表现、人工地震勘查、断裂绝对年龄测定、跨断裂水准测量以及断裂与地震的关系等资料的综合分析与研究,认为该段是一条活动性不均一,其活动强度不大的区域性构造。
By means of analysis and study for the Landforms on the different section,man-made earthquake exploration,fracture absolute age measure,across fracture leveling measure,relationship between fracture and earthquake,it was consided that hunhe fracture (Shenyang-Fushun section)is an areal structure with nonuniform activity and weak strength.
出处
《东北地震研究》
2004年第1期25-32,共8页
Seismological Research of Northeast China
