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Three Component Seismogram Analysis: A Case Study of the M = 7.7 South Java, Indonesia Earthquake on July 17, 2006 and Changes in Coulomb Stress and Seismicity Rate

机译:三种组分地震图分析:2006年7月17日南爪哇南爪哇南爪哇省南爪哇省的案例研究,以及库仑应力和地震率的变化

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After An earthquake event in South Java, Indonesia on July 17th, 2006 at 08:20:38.4 UTC (Universal Time Coordinate) has been investigated to estimate the earthquake’s source parameters. Seismogram data were obtained from five stations in the vicinity of the epicenter, with distancesof less than 20°. All analyzed data are waveforms withthree components. The method for estimating source parameters is a combination of iterative deconvolution and discrete wavenumber (DWN) for local data. The results show that the reduction in variance between the observed seismogramsand synthetic sets for all stations is 69.97%. This indicates that the estimation results (for hypocenter, seismic moment, moment tensor and rupture direction) are suitable for describing the earthquake source point. The source parameters of this event are its hypocenter (?10.28°,107.78°, 23 km), seismic moment (4.525×10~(20) Nm), moment tensor and rupture direction, which can be used to describe the focal mechanism of the earthquake. Almost all of the aftershock epicenters after the main earthquake on July 17th, 2006 were located within an area thatexperienced an increase in Coulomb stress. This indicates that an increase in Coulomb stress could trigger aftershocks in South Java, and there is the positive correlation between change in Coulomb stress and change in seismicity rate.
机译:在2006年7月17日的印度尼西亚在南爪哇举行的地震事件发生之后,在08:20:38.4 UTC(环球时坐标)已经调查估算地震的源参数。地震图数据是从震中附近的五个站获得的,距离小于20°。所有分析的数据都是带有三种组件的波形。估计源参数的方法是迭代解卷积和离散波数(DWN)的组合,用于本地数据。结果表明,所有车站的观察到地震图和合成套之间的变化的减少为69.97%。这表明估计结果(用于低速度,地震时刻,时刻张力和破裂方向)适合于描述地震源点。该事件的源参数是其次静脉(?10.28°,107.78°,23km),地震时刻(4.525×10〜(20)Nm),时刻张量和破裂方向,可用于描述焦点机制地震。 2006年7月17日主要地震发生后几乎所有的余震震中都位于一个区域内,在一个区域内的Coulomb压力增加。这表明库仑应力的增加可以触发南爪哇的余震,并且库仑应力变化与地震率变化之间存在正相关性。

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