根据日俄共同地震观测2007年8月2日发生的库页岛西南海域地震(m_6.4)的余震活动

一柳 昌義, 高橋 浩晃, 前田 宜浩, 笠原 稔, 宮町 宏樹, 平野 舟一郎, Sen Rak Se, M. Valentin, Kim Chun Ung
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引用次数: 0

摘要

2007年8月2日,俄罗斯远东库页岛西南海岸发生了MJMA 6.4级的中等地震。在位于余震区的涅维尔斯克市,有2人死亡,240多座建筑受损(我们称此事件为2007年涅维尔斯克地震)。自2003年以来,我们在库页岛南部运行了一个时间地震台网,该台网由10个站点组成,配有短周期传感器和16位记录器。这个密集的网络很好地记录了这次地震和随后的余震序列。根据746次p波到达时间(包括余震数据)估计的1-D p波速度结构计算了初始余震震源。为了获得更精确的余震分布,我们采用了双差震源测定方法。确定的余震震源具有以下特点:(1)震区北部和中部震源沿海岸向海上分布,呈NE-SW方向;(2)震区南部震源向陆地方向转变,呈NNW-SSE方向。最南部的部分与涅维尔斯克市相交,涅维尔斯克市遭受了严重的破坏。2006年8月17日,2006年戈莫扎德斯科地震(MJMA 5.9)发生在2007年涅维尔斯克地震的东南余震区附近。与2007年的地震相比,2006年的地震序列发生在更深的区域。我们研究了2006年事件产生的库仑失效函数的变化,得出2006年事件对2007年事件发生的影响较小的结论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
日露共同地震観測による2007年8月2日に発生したサハリン南西沖の地震(M_ 6.4)の余震活動
On August 2, 2007, an MJMA 6.4 moderate earthquake occurred off the southwest coast of Sakhalin Island, far eastern Russia. In the city of Nevelsk, situated just in the aftershock region, two people were killed and more than 240 buildings were damaged (we call this event as the 2007 Nevelsk earthquake). We have operated a temporal seismological network in southern Sakhalin consisted in ten stations with short-period sensors and 16-bit recorders since 2003. This dense network well recorded this earthquake and the following aftershock sequence. Initial aftershock hypocenters were calculated using a 1-D P-wave velocity structure that was estimated from 746 P-wave arrival times, including data from the aftershocks. To obtain a more precise aftershock distribution, we applied a double-difference hypocenter determination method. The well-determined aftershock hypocenters shows the following features; (1) in the northern and central parts of aftershock region, epicenters were distributed in the sea along the coast with NE-SW direction, (2) while in the southern part of aftershock region trend of epicenters changed toward land with NNW-SSE direction. This southern most part intersects the city of Nevelsk where severe damage occurred. On August 17, 2006, the 2006 Gomozavodskoe earthquake (MJMA 5.9) occurred near the southeastward aftershock region of the 2007 Nevelsk earthquake. The 2006 earthquake sequence was occurred deeper area as compared to the 2007 event. We examine the change in Coulomb failure function produced by the 2006 event and conclude that the 2006 event has less influence on occurrence of the 2007 event.
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