首页 | 本学科首页   官方微博 | 高级检索  
     

沂沭断裂带安丘-莒县断裂安丘-朱里段几何结构与活动特征
引用本文:王志才,贾荣光,孙昭民,石荣会,晁洪太. 沂沭断裂带安丘-莒县断裂安丘-朱里段几何结构与活动特征[J]. 地震地质, 2005, 27(2): 212-220. DOI: ISSN:0253-4967.0.2005-02-003
作者姓名:王志才  贾荣光  孙昭民  石荣会  晁洪太
作者单位:1. 中国地震局地质研究所,北京,100029;山东省地震工程研究院,济南,250014
2. 山东省地震工程研究院,济南,250014
基金项目:山东省科技攻关项目;山东省地震局资助项目;中国地震局地质研究所项目
摘    要:安丘-莒县断裂是沂沭断裂带最主要的活动断裂,对强震的发生具有明显的控制作用。该断裂的安丘—朱里段由南流段、双官—眉村段和朱里段3条右阶斜列的次级断裂所组成,以右旋走滑活动为主,兼有正断或逆冲活动分量;其最新活动时代推断为晚更新世—全新世早期。根据断裂活动性的最新研究成果,认为在莒县至昌邑之间安丘-莒县断裂仍是占主导地位的活动断裂,与公元前70年安丘7级地震的发生具有密切关系

关 键 词:断裂活动性  安丘-莒县断裂  安丘—朱里段  安丘7级地震
文章编号:0253-4967(2005)02-0212-09
修稿时间:2004-08-11

GEOMETRY AND ACTIVITY OF THE ANQIU-ZHULI SEGMENT OF THE ANQIU-JUXIAN FAULT IN THE YISHU FAULT ZONE
WANG Zhi-cai,JIA Rong-guang,SUN Zhao-min,SHI Rong-hui,CHAO Hong-tai. GEOMETRY AND ACTIVITY OF THE ANQIU-ZHULI SEGMENT OF THE ANQIU-JUXIAN FAULT IN THE YISHU FAULT ZONE[J]. Seismology and Geology, 2005, 27(2): 212-220. DOI: ISSN:0253-4967.0.2005-02-003
Authors:WANG Zhi-cai  JIA Rong-guang  SUN Zhao-min  SHI Rong-hui  CHAO Hong-tai
Abstract:The Yishu Fault zone is a part of the Tanlu Fault zone that passes through Shandong Province and the northern area of Jiangsu. It is composed of 5 nearly parallel faults among which the Anqiu-Juxian Fault is the most important and prominent active fault since late Pleistocene and is usually considered to be the seismogenic fault of the 70 BC M 7 Anqiu earthquake and the 1668 AD M 8~1/_2 Tancheng earthquake. By detailed research in recent years, e.g. the active fault mapping implemented during the “Eighth Fi
Keywords:fault activity   Anqiu-Juxian Fault   Anqiu-Zhuli segment   the M 7 Anqiu earthquake
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号