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This seismicity shows a systematic spatiotemporal evolution, but little is known of the heterogeneity in crustal structure in this region, or its influence on the evolution of the seismicity. Here, we elucidate a high-resolution model of crustal structure in this region and determine precise hypocenter locations. Hypocenters in Ibaraki Prefecture reveal a planar earthquake alignment dipping SW at ∼45°, whereas those in Fukushima Prefecture show a more complex distribution, consisting of conjugate sets of aligned small earthquakes. On the north of the hypocenter of the largest earthquake in the sequence (the M7.0 Iwaki earthquake), we imaged a high-velocity body at shallow depths that lacks aftershock seismicity. Based on fault source models, the large-slip region of the Iwaki earthquake is situated along a zone that roughly coincides with this high-velocity body. We delineated a separate low-velocity anomaly directly beneath the hypocenter of the Iwaki earthquake, indicating crustal fluids in this region. We hypothesize that strong crust underwent structural failure due to the infiltration of crustal fluids into the seismogenic zone from deeper levels, causing the Iwaki earthquake. © 2013. American Geophysical Union. 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  1. 防災科研関係論文

Imaging the source regions of normal faulting sequences induced by the 2011 M9.0 Tohoku-Oki earthquake

https://nied-repo.bosai.go.jp/records/4070
https://nied-repo.bosai.go.jp/records/4070
dc2269e8-3d21-4cfb-9221-b2635110c49b
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Imaging the source regions of normal faulting sequences induced by the 2011 M9.0 Tohoku-Oki earthquake
著者 Aitaro Kato

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en Aitaro Kato

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Toshihiro Igarashi

× Toshihiro Igarashi

en Toshihiro Igarashi

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Kazushige Obara

× Kazushige Obara

en Kazushige Obara

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Shinichi Sakai

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en Shinichi Sakai

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Tetsuya Takeda

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en Tetsuya Takeda

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Atsushi Saiga

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en Atsushi Saiga

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Takashi Iidaka

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en Takashi Iidaka

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Takaya Iwasaki

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en Takaya Iwasaki

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Naoshi Hirata

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en Naoshi Hirata

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Kazuhiko Goto

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en Kazuhiko Goto

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Hiroki Miyamachi

× Hiroki Miyamachi

en Hiroki Miyamachi

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Takeshi Matsushima

× Takeshi Matsushima

en Takeshi Matsushima

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Atsuki Kubo

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en Atsuki Kubo

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Hiroshi Katao

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en Hiroshi Katao

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Yoshiko Yamanaka

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en Yoshiko Yamanaka

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Toshiko Terakawa

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en Toshiko Terakawa

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Haruhisa Nakamichi

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en Haruhisa Nakamichi

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Takashi Okuda

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en Takashi Okuda

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Shinichiro Horikawa

× Shinichiro Horikawa

en Shinichiro Horikawa

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Noriko Tsumura

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en Noriko Tsumura

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Norihito Umino

× Norihito Umino

en Norihito Umino

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Tomomi Okada

× Tomomi Okada

en Tomomi Okada

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Masahiro Kosuga

× Masahiro Kosuga

en Masahiro Kosuga

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Hiroaki Takahashi

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Takuji Yamada

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抄録
内容記述タイプ Other
内容記述 Intense swarm-like seismicity associated with shallow normal faulting was induced in Ibaraki and Fukushima prefectures, Japan, following the 2011 Tohoku-Oki earthquake. This seismicity shows a systematic spatiotemporal evolution, but little is known of the heterogeneity in crustal structure in this region, or its influence on the evolution of the seismicity. Here, we elucidate a high-resolution model of crustal structure in this region and determine precise hypocenter locations. Hypocenters in Ibaraki Prefecture reveal a planar earthquake alignment dipping SW at ∼45°, whereas those in Fukushima Prefecture show a more complex distribution, consisting of conjugate sets of aligned small earthquakes. On the north of the hypocenter of the largest earthquake in the sequence (the M7.0 Iwaki earthquake), we imaged a high-velocity body at shallow depths that lacks aftershock seismicity. Based on fault source models, the large-slip region of the Iwaki earthquake is situated along a zone that roughly coincides with this high-velocity body. We delineated a separate low-velocity anomaly directly beneath the hypocenter of the Iwaki earthquake, indicating crustal fluids in this region. We hypothesize that strong crust underwent structural failure due to the infiltration of crustal fluids into the seismogenic zone from deeper levels, causing the Iwaki earthquake. © 2013. American Geophysical Union. All Rights Reserved.
言語 en
書誌情報 en : Geophysical Research Letters

巻 40, 号 2, p. 273-278
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/grl.50104
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