浑河断裂(沈阳～抚顺段)活动性研究  

ACTIVITY RESEARCH ON HUNHE FRACTURE (SHENYANG～FUSHUN SECTION)

作　　者：吴明大[1] 钟以章[1] 高常波[1] 万波[1] 郑双成[1] 

机构地区：[1]辽宁省地震局,沈阳110031

出　　处：《东北地震研究》2004年第1期25-32,共8页Seismological Research of Northeast China

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.

关 键 词：浑河断裂 地震地震 地震勘查 年龄测定 地貌 

分 类 号：P315.5[天文地球—地震学]