摘要
印尼8.7级地震发生后,在不到2个月时间内,在中国大陆相继发生了3次后续中强地震(2004年12月26日云南双柏MS5.1地震、2005年1月26日云南思茅MS5.1地震、2005年2月15日新疆乌什MS6.2地震),印尼地震和这3次后续地震是否存在触发关系?计算了印尼地震在3次后续地震破裂面上的动库仑应力变化和静库仑应力变化。静应力变化量小,低于一般认为的触发阈值(0.01 MPa);动应力变化峰值为10-1MPa,可能是这3次后续地震的触发因素。
In two months after Indonesia Ms8. 7 earthquake, three moderately strong earthquakes (December 26, 2004 Ms5. 1 Shuangbai earthquake, January 26, 2005 Ms5.1 Simao earthquake and February 15, 2005 Ms6.2 Wushi earthquake) occurred in China" mainland. Is there triggering relation between Indonesia Ms8. 7 Earthquake and the three subsequent earthquakes? In this article we calculate the static and dynamic Coulomb stress changes in failure planes of the three subsequent earthquakes for Indonesia Ms8. 7 Earthquake. The value of static stress change is smaller than the threshold one of triggering value (0.01 MPa);The peak change of dynamic stress is about 10 1 MPa. So the change of dynamic stress is probably the triggering factor of the three subsequent earthquakes.
出处
《地震》
CSCD
北大核心
2006年第3期26-36,共11页
Earthquake
基金
地震科学联合基金项目(103073)
中国数字地震观测网络工程城市活断层实验探测项目
关键词
动应力触发
库仑破裂应力
印尼Ms8.7地震
Dynamic stress triggering
Coulomb failure stress
Indonesia Ms8.7 Earthquake