苏皖交界北西向断裂构造地震危险性分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
苏皖交界近年来不断有地震发生,2012年7月发生了Ms4.9级地震,造成了一定的破坏,其社会影响大。在此震情形势下,本文通过分析苏皖交界北西向断裂构造的活动特征、北西向断裂构造与历史破坏性地震及现代2.0级以上地震间的关系,认为苏皖交界区域沿扬州—六合—高邮—盱眙—洪泽—带被北西向的自来桥—来安断裂和无锡—宿迁断裂所夹持的区域,未来有发生Ms5.0级地震的构造背景,应关注其未来地震危险性。
Earthquakes occur in the junction of Anhui and Jiangsu province recently.The Ms 4.9 earthquake appeared in July 2012 and destroyed many houses with a wide social influence.By the analysis of the north-west striking fault structure’s active characters and the relation between the north-west striking fault structure and destructive earthquakes as well as the earthquakes whose magnitude are more than 2,the region is thought as seismic risk area with the magnitude of 5 along Yangzhou,Liuhe,Gaoyou,Xuyi and Hongze,which is worth of attention.
引文
[1]谢瑞征,徐徐,黄伟生.苏浙皖沪地区中强地震潜在震源区判定标志的研讨[J].地震学刊,1997,(1):11-20.
    [2]郭爱香,林怀存,石玉燕.鲁苏皖交界地区地震活动特点浅析[J].华北地震科学,2003,21(1):32-38.
    [3]周本刚,沈得秀.地震安全性评价中若干地震地质问题探讨[J].震灾防御技术,2006,1(2):113-120.
    [4]郭良迁,黄立人.苏鲁皖地区现代构造活动性研究[J].大地测量与地球动力学,2008,28(4):17-24.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心