|本期目录/Table of Contents|

[1]王 俊,孙业君,詹小艳,等.2005年江西九江—瑞昌MS5.7地震破裂参数及余震静态应力触发研究*[J].地震研究,2011,34(01):0.
 WANG Jun,SUN Ye-jun,ZHAN Xiao-yan,et al.Investigation on Rupture Parameters of the 2005 MS5.7 Jiujiang-Ruichang, Jiangxi Earthquake and Static Stress Triggering of Its Aftershocks[J].Journal of Seismological Research,2011,34(01):0.
点击复制

2005年江西九江—瑞昌MS5.7地震破裂参数及余震静态应力触发研究*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
34
期数:
2011年01期
页码:
0
栏目:
出版日期:
2011-03-09

文章信息/Info

Title:
Investigation on Rupture Parameters of the 2005 MS5.7 Jiujiang-Ruichang, Jiangxi Earthquake and Static Stress Triggering of Its Aftershocks
作者:
王 俊1孙业君1詹小艳1霍祝青1阮 祥2郑江蓉2
(1.江苏省地震局,南京 210014; 2.四川省地震局,成都 610041)
Author(s):
WANG Jun1SUN Ye-jun1ZHAN Xiao-yan1HUO Zhu-qing1RUAN Xiang2ZHENG Jiang-rong1
(1.Earthquake Administration of Jiangsu Province,Nanjing 210014,Jiangsu,China)(2.Earthquake Administration of Sichuan Province,Chengdu 610041,Sichuan,China)
关键词:
九江—瑞昌MS5.7地震 震源破裂参数 静态库仑应力 余震触发
Keywords:
Jiujiang-Ruichang MS5.7 earthquake source rupture parameters static Coulomb failure stress triggering of aftershocks
分类号:
P315.3+3
DOI:
-
摘要:
根据地震破裂过程中的多普勒效应,利用多台波谱参数推算九江—瑞昌MS5.7地震的震源破裂参数,得到主震的破裂方位角φ0≈319.6°,破裂速度约为2.3 km/s,用最小二乘法拟合的相关系数极值约为0.80。在此基础上,分别计算了主震在4.8级强余震的两个节面上的静态库仑应力变化量,结果显示:主震在4.8级余震节面Ⅰ、Ⅱ上的静态库仑应力变化均为正值,分别为0.48 MPa和0.02 MPa。主震在节面Ⅰ、Ⅱ上产生的静态库仑应力的变化十分接近。应力增加的区域主要位于
Abstract:
According to the Doppler Effect in the earthquake rupture process,we use the multi-station spectrum to calculate rupture parameters of the Jiujiang-Ruichang MS5.7 earthquake in Jiangxi.We get the results that the rupture azimuth is about 319.6°,the rupture velocity is about 2.3 km/s,and the fitted minimum correlation-coefficient is about 0.80 by minimum squares.And on this basis,We calculate the variation of static Coulomb stress separately in the two rupture planes of the MS4.8 aftershock.The results show that the variation of the static Coulomb stress separately on two nodal planes are positive,the values are about 0.48 MPa and 0.02 MPa respectively.The variations of static Coulomb stress on nodalⅠ and Ⅱ are very close.Stress-increasing area is mainly located on the right of the main earthquake fault.Stress-reducing area is mainly located to the south of the epicenter.Most of the aftershocks occur in the static Coulomb stress-increasing region,especially on the nodal.This shows the Coulomb failure stress variation caused by the main shock has an important role in triggering of the MS4.8 aftershock,and also conductive to majori aftershocks' occurrence.

参考文献/References:

-

备注/Memo

备注/Memo:
收稿日期:2010-03-08
基金项目:中国地震局2009年度“三结合”课题(NO.09707)和中国地震局“十一五”科技支撑计划(2006BAC01B03-03-01)共同资助.

更新日期/Last Update: 2011-03-30