JpGU-AGU Joint Meeting 2017

講演情報

[EE] 口頭発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS08] [EE] Earthquake Modeling and Simulation

2017年5月22日(月) 13:45 〜 15:15 A02 (東京ベイ幕張ホール)

コンビーナ:福山 英一(防災科学技術研究所)、John B Rundle(University of California Davis)、深畑 幸俊(京都大学防災研究所)、座長:安藤 亮輔(東京大学大学院理学系研究科)、座長:深畑 幸俊(京都大学防災研究所)

14:00 〜 14:15

[SSS08-08] Simultaneous estimation of the dip angles and slip distribution on the two active faults of the 2016 Kumamoto earthquak

*深畑 幸俊1橋本 学1 (1.京都大学防災研究所)

キーワード:The 2016 Kumamoto earthquake, weak nonlinear inversion analysis, ABIC

At the 2016 Kumamoto earthquake, surface ruptures were observed not only along the Futagawa fault, where main ruptures occurred, but also along the Hinagu fault. To estimate the slip distribution on these faults, we extend a method of non-linear inversion analysis (Fukahata and Wright 2008) to a two-faults system. With the method of Fukahata and Wright (2008) we can simultaneously determine the optimal dip angle of a fault and the slip distribution on it, based on Akaike's Bayesian Information Criterion (ABIC) by regarding the dip angle as an hyperparameter. By inverting the InSAR data with the developed method, we obtain the dip angles of the Futagawa and Hinagu faults as 61º ± 6º and 74º ± 12º, respectively. The slip on the Futagawa fault is mainly strike slip. The largest slip on it is over 5 m around the center of the model fault (130.9º in longitude) with a significant normal slip component. The slip on the Futagawa fault quickly decreases to zero beyond the intersection with the Hinagu fault. On the other hand, the slip has a local peak just inside Aso caldera, which would be a cause of severe damage in this area. A relatively larger reverse fault slip component on a deeper part around the intersection with Aso caldera suggests that something complicated happened there. The slip on the Hinagu fault is almost a pure strike slip with a peak of about 2.4 m. The developed method is useful in clarifying the slip distribution, when a complicated rupture like the Kumamoto earthquake happens in a remote area.