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  1. 防災科研関係論文

Stress rotations due to the M6.5 foreshock and M7.3 main shock in the 2016 Kumamoto, SW Japan, earthquake sequence

https://nied-repo.bosai.go.jp/records/4029
https://nied-repo.bosai.go.jp/records/4029
a530c3f2-cde0-49a8-9ba2-98b5389184c5
Item type researchmap(1)
公開日 2024-11-18
タイトル
言語 en
タイトル Stress rotations due to the M6.5 foreshock and M7.3 main shock in the 2016 Kumamoto, SW Japan, earthquake sequence
言語
言語 eng
著者 Keisuke Yoshida

× Keisuke Yoshida

en Keisuke Yoshida

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Akira Hasegawa

× Akira Hasegawa

en Akira Hasegawa

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Tatsuhiko Saito

× Tatsuhiko Saito

en Tatsuhiko Saito

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Youichi Asano

× Youichi Asano

en Youichi Asano

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Sachiko Tanaka

× Sachiko Tanaka

en Sachiko Tanaka

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Kaoru Sawazaki

× Kaoru Sawazaki

en Kaoru Sawazaki

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Yumi Urata

× Yumi Urata

en Yumi Urata

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Eiichi Fukuyama

× Eiichi Fukuyama

en Eiichi Fukuyama

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抄録
内容記述タイプ Other
内容記述 A shallow M7.3 event with a M6.5 foreshock occurred along the Futagawa-Hinagu fault zone in Kyushu, SW Japan. We investigated the spatiotemporal variation of the stress orientations in and around the source area of this 2016 Kumamoto earthquake sequence by inverting 1218 focal mechanisms. The results show that the sigma 3 axis in the vicinity of the fault plane significantly rotated counterclockwise after the M6.5 foreshock and rotated clockwise after the M7.3 main shock in the Hinagu fault segment. This observation indicates that a significant portion of the shear stress was released both by the M6.5 foreshock and M7.3 main shock. It is estimated that the stress release by the M6.5 foreshock occurred in the shallower part of the Hinagu fault segment, which brought the stress concentration in its deeper part. This might have caused the M7.3 main shock rupture mainly along the deeper part of the Hinagu fault segment after 28h.
言語 en
書誌情報 en : GEOPHYSICAL RESEARCH LETTERS

巻 43, 号 19, p. 10097-10104, 発行日 2016-10
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 1944-8007
DOI
関連識別子 10.1002/2016GL070581
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