长江破碎带的研究过程及最新认识  

Recent Study of Changjiang Fault Zone

作　　者：侯康明[1] 宗开红[2] 郭江宁[1] 熊振[1] 李丽梅[1] 周彩霞[1] 蒋波[2] 

机构地区：[1]江苏省地震局,南京210014 [2]江苏省地质调查研究院,南京210014

出　　处：《震灾防御技术》2007年第4期331-338,共8页Technology for Earthquake Disaster Prevention

基　　金：国家"十五"重大建设项目;中国地震活断层探测技术系统分项目(1-4-10);南京市活动断层探测及地震危险性评价项目

摘　　要：本文依据南京市及其附近区域(活动断层探测目标区范围)所开展的浅层人工地震探测、槽探、钻探,以及第四纪地层划分、新年代学测试数据等多学科资料,综合评价了长江破碎带的最新活动年代、活动性质、断层相关参数及其与地震活动关系方面的最新认识。Changjiang fault zone, also called Mufushang-Jiaoshan fault, is a famous fault that is located at the southern bank of the Changjiang river around Nanjing downtown area. Striking in about east-west orientation with the north trending, this fault is near 100kra long and is featured by normal fault mode. At both ends of the fault, there occurred earthquakes with magnitude of 5-6 in the past. Based on the analysis from shallow artificial seismic exploration, trough study, drilling exploration and application of dating techniques, this paper provides the most-up-to-date results regarding to the activity of Changjiang fault, such as most recent active time, faulting mode, the related active parameters and relation to the seismic activity.

关 键 词：长江破碎带 断层活动性 第四纪地层划分 联合钻探剖面 断层地质剖面 

分 类 号：P315[天文地球—地震学]