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  1. 防災科研関係論文

Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (M7.3)

https://nied-repo.bosai.go.jp/records/4048
https://nied-repo.bosai.go.jp/records/4048
0444cd79-3ecc-4935-a0b4-f2f1433985b0
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (M7.3)
言語
言語 eng
著者 Satoshi Matsumoto

× Satoshi Matsumoto

en Satoshi Matsumoto

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Yusuke Yamashita

× Yusuke Yamashita

en Yusuke Yamashita

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Manami Nakamoto

× Manami Nakamoto

en Manami Nakamoto

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Masahiro Miyazaki

× Masahiro Miyazaki

en Masahiro Miyazaki

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Shinichi Sakai

× Shinichi Sakai

en Shinichi Sakai

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Yoshihisa Iio

× Yoshihisa Iio

en Yoshihisa Iio

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Hiroshi Shimizu

× Hiroshi Shimizu

en Hiroshi Shimizu

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Kazuhiko Goto

× Kazuhiko Goto

en Kazuhiko Goto

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Tomomi Okada

× Tomomi Okada

en Tomomi Okada

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Mako Ohzono

× Mako Ohzono

en Mako Ohzono

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Toshiko Terakawa

× Toshiko Terakawa

en Toshiko Terakawa

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Masahiro Kosuga

× Masahiro Kosuga

en Masahiro Kosuga

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Masayuki Yoshimi

× Masayuki Yoshimi

en Masayuki Yoshimi

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Youichi Asano

× Youichi Asano

en Youichi Asano

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抄録
内容記述タイプ Other
内容記述 Fault behavior during an earthquake is controlled by the state of stress on the fault. Complex coseismic fault slip on large earthquake faults has recently been observed by dense seismic networks, which complicates strong motion evaluations for potential faults. Here we show the three-dimensional prestress field related to the 2016 Kumamoto earthquake. The estimated stress field reveals a spatially variable state of stress that forced the fault to slip in a direction predicted by the "Wallace and Bott Hypothesis." The stress field also exposes the pre-condition of pore fluid pressure on the fault. Large coseismic slip occurred in the low-pressure part of the fault. However, areas with highly pressured fluid also showed large displacement, indicating that the seismic moment of the earthquake was magnified by fluid pressure. These prerupture data could contribute to improved seismic hazard evaluations.Plain Language Summary The three-dimensional prestress field around the 2016 Kumamoto earthquake controlled fault behavior of the earthquake. The estimated heterogeneous state of stress on the fault forced the fault to slip in the direction predicted. The stress field also exposed the precondition of pore fluid pressure on the fault. Large coseismic slip occurred not only at the low-pressure part of the fault but also highly pressured part. It indicates that the seismic moment of the earthquake was magnified by fluid pressure. These prerupture data could contribute to upgrading seismic hazard evaluation.
言語 en
書誌情報 en : GEOPHYSICAL RESEARCH LETTERS

巻 45, 号 2, p. 637-645
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 10.1002/2017GL075725
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