文章基本信息

标题：Testing the Coulomb stress triggering hypothesis for three recent megathrust earthquakes
本地全文：下载
作者：Takeo Ishibe ; Takeo Ishibe ; Yosihiko Ogata 等
期刊名称：Geoscience Letters
电子版ISSN：2196-4092
出版年度：2017
卷号：4
期号：1
页码：1-11
DOI：10.1186/s40562-017-0070-y
语种：English
出版社：Springer
摘要：Abstract We test the static Coulomb stress triggering hypothesis for three recent megathrust earthquakes (the 2004 Sumatra–Andaman earthquake, the 2010 Maule earthquake, and the 2011 Tohoku-Oki earthquake) using focal mechanism solutions for actual earthquakes as receiver faults to calculate Coulomb stress changes. For the 2004 Sumatra–Andaman and 2011 Tohoku-Oki earthquakes, the median values of the Coulomb stress changes for 100 consecutive earthquakes revealed temporal changes from approximately zero before the megathrust earthquake to significant positive values following the mainshock, followed by decay over time. Furthermore, the ratio of the number of positively to negatively stressed receiver faults increased after the megathrust. These results support the triggering hypothesis that the static stress changes imparted by megathrust earthquakes cause seismicity changes. This is in contrast to the results of a previous study that used optimally orientated receiver faults to calculate Coulomb stress changes, and this difference indicates the importance of considering the spatial and temporal heterogeneities of receiver fault distributions. For the 2010 Maule earthquake, however, the results are strongly dependent on fault-slip models. Since most receiver faults are concentrated in the mainshock source region, slip models significantly affect the computed Coulomb stress changes and sometimes cause anomalous stress concentrations along the edge of each sub-fault.
关键词：KeywordsEnCoulomb stress changes2004 Sumatra–Andaman earthquake2010 Maule earthquake2011 Tohoku-Oki earthquakeHeterogeneity of receiver fault mechanisms