山东沿黄河断裂带的地震地质特征  

THE SEISMOGEOLOGICAL CHARACTERISTICS OF THE YELLOW RIVER FRACTURE ZONE IN SHANDONG PROVINCE

作　　者：刘西林[1] 申旭华 

机构地区：[1]山东省地震局

出　　处：《华北地震科学》1993年第3期55-61,共7页North China Earthquake Sciences

摘　　要：通过对山东沿黄河地质、地貌、钻探、物探和地震活动性等方面的分析,山东沿黄河存在一条隐伏深大断裂带。论述了该带的分段特征、构造上深部与浅部的一致性和非一致性及其活动性质。沿黄河断裂带是山东地区的一条重要地震活动带,深入研究该断裂带的地震地质及其新构造活动特征对本区的地震监测预报和黄河防灾都具有重要意义。Based on the analysis of geology, physiognomy, boring, physical exploration, seismic activity etc. along the Yellow River, the authors think there is a deep and large hidden fracture zone along the Yellow River and discuss the characteristics of the segments, the consistence and nonconsistence characteristics of deep and shallow structures and their activity characteristics. Along the Yellow River fracture zone is an important belt of seismic activity in Shandong region. It is significant to deeply study the seismogeological and new tectonic activity characteristics along the Yellow River fracture zone for earthquake monitoring and prediction and the Yellow River defence of this region.

关 键 词：黄河 断裂带 地震 地质特征 

分 类 号：P315.2[天文地球—地震学]