Abstrak

We studied the seismicity rate increase in the Kanto region around Tokyo following the 2011 Tohoku-Oki earthquake (Mw 9.0) to examine whether this increase was correlated withthe static increases in the Coulomb failure function (CFF) of the Tohoku-Oki earthquake sequence. Because earthquakes in the Kanto region exhibit various focal mechanisms, the receiver faults for the CFF were assumed to be the focal mechanism solutions for nearly 19000 earthquakes that previously occurred. Our results showed that the number of earthquakes for which the mechanism solutions had a positive CFF (∼12 000) is much larger than those that had a negative CFF (∼2000). Comparison of the CFF values for earthquakes before and after the Tohoku-Oki earthquake showed that the latter had more positive values; this supports the hypothesis that the coseismic stress change transferred from the Tohoku-Oki earthquake sequence is the major contributing factor to the increased seismicity rate in the Kanto region. Key words: Seismicity and tectonics; Statistical seismology; Asia.