日本地球惑星科学連合2015年大会

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セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS27] 地震予知・予測

2015年5月24日(日) 10:00 〜 10:45 103 (1F)

コンビーナ:*中島 淳一(東北大学大学院理学研究科附属地震・噴火予知研究観測センター)、座長:前田 憲二(気象研究所)

10:00 〜 10:15

[SSS27-01] 地震発生の予測可能性があるかないか?~前震活動の統計的性質に着目した検討

*鴨川 仁1田中 利佳1織原 義明1橋本 哲1 (1.東京学芸大学教育学部物理学科)

キーワード:地震, 前震, 余震

The relation between the size of earthquake preparation zone and the magnitude of forthcoming earthquake is different between nucleation and domino-like cascade models. The former model indicates that the magnitude is predictable before the mainshock of the earthquake, because the preparation zone is proportional to the rupture area. One the other hand, the latter indicates that the magnitude is unpredictable, because the rupture consisting of sequence of tiny earthquakes is unknown to terminate. Since this issue is still controversial, we would like to verify the two models using the methodology proposed by Lippiello et al. (Scientific reports, 2012). In the analysis, spatial occurrence rates of the foreshock and the aftershock are statistically compared. The results show that both the rates are similar and the distribution of the rates versus the epicentral distance depends on the magnitude of the mainshock. From the interpretation of these results, the nucleation model seems reliable.