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  1. 防災科研関係論文

Rupture process of the largest aftershock of the M 9 Tohoku-oki earthquake obtained from a back-projection approach using the MeSO-net data

https://nied-repo.bosai.go.jp/records/5886
https://nied-repo.bosai.go.jp/records/5886
cd6c49e2-6bfa-4f82-b24e-31f13e177708
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Rupture process of the largest aftershock of the M 9 Tohoku-oki earthquake obtained from a back-projection approach using the MeSO-net data
言語
言語 eng
著者 Ryou Honda

× Ryou Honda

en Ryou Honda

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Yohei Yukutake

× Yohei Yukutake

en Yohei Yukutake

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Hiroshi Ito

× Hiroshi Ito

en Hiroshi Ito

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Masatake Harada

× Masatake Harada

en Masatake Harada

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Tamotsu Aketagawa

× Tamotsu Aketagawa

en Tamotsu Aketagawa

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Akio Yoshida

× Akio Yoshida

en Akio Yoshida

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Shin'ichi Sakai

× Shin'ichi Sakai

en Shin'ichi Sakai

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Shigeki Nakagawa

× Shigeki Nakagawa

en Shigeki Nakagawa

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Naoshi Hirata

× Naoshi Hirata

en Naoshi Hirata

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Kazushige Obara

× Kazushige Obara

en Kazushige Obara

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Makoto Matsubara

× Makoto Matsubara

en Makoto Matsubara

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Hisanori Kimura

× Hisanori Kimura

en Hisanori Kimura

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抄録
内容記述タイプ Other
内容記述 The largest aftershock (M-w 7.8) of the giant M 9.0 Tohoku-oki earthquake occurred near the coast of Ibaraki Prefecture about thirty minutes after the main shock. We have imaged the rupture process of the M-w 7.8 earthquake by back-projection of waveform data from the Metropolitan Seismic Observation network (MeSO-net). Original acceleration seismograms were integrated. They were then band-pass filtered in the frequency range of 0.1-1.0 Hz. We assumed a fault plane on the plate boundary with a dimension of 115 km x 175 km, and this was divided into 112 subfaults. Travel times from each of the subfaults to observation sites were calculated by using a 3-D velocity structure model. Applying the restrictions that the rupture velocity is smaller than 4 km/s and the rupture duration on each subfault is less than 25 s, we obtained a rupture propagation image by projecting the power of the stacked waveforms. Propagation of the rupture toward north and east was suppressed by the existence of those areas that had radiated a large seismic energy at the main shock occurrence, or at the occurrence of the M 7.0 earthquake in 2008. The westward propagation of the rupture stopped at the area where the Philippine Sea plate lies over the Pacific plate.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 65, 号 8, p. 917-921, 発行日 2013
出版者
言語 en
出版者 TERRA SCIENTIFIC PUBL CO
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.5047/eps.2013.01.003
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