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  1. 防災科研関係論文

Spatiotemporal Change in the Stress State Around the Hypocentral Area of the 2016 Kumamoto Earthquake Sequence

https://nied-repo.bosai.go.jp/records/4595
https://nied-repo.bosai.go.jp/records/4595
0c37a8b4-eb77-4705-8334-97ad98ddb813
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Spatiotemporal Change in the Stress State Around the Hypocentral Area of the 2016 Kumamoto Earthquake Sequence
言語
言語 eng
著者 Ayaho Mitsuoka

× Ayaho Mitsuoka

en Ayaho Mitsuoka

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Azusa Shito

× Azusa Shito

en Azusa Shito

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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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Shin-ichi Sakai

× Shin-ichi Sakai

en Shin-ichi 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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Yoshiko Yamanaka

× Yoshiko Yamanaka

en Yoshiko Yamanaka

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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 For understanding the physical condition of earthquake generation, we estimated the deviatoric stress fields and fault planes of the large earthquakes in the hypocentral area of the 2016 Kumamoto earthquake sequence, central Kyushu, Japan. We analyzed precise hypocenters and their focal mechanism tensors from 1993 to 2017 and found the complex fault planes of the largest foreshock and the mainshock during the sequence. The faults of large earthquakes could not be detected from the preceding high seismic activity in the area to the mainshock. The analyses of the deviatoric stress tensors obtained from pre- and post-sequence seismic moment tensor data revealed the temporal change in the deviatoric stress field at the vicinity of the hypocenters of the largest foreshock and the mainshock. Because of this temporal change, we found that the stress level of the deviatoric stress field in this region is the same level as the co-seismic stress change caused by the two large earthquakes. We attempted to estimate the differential stress at the region using a new method, which can be applied to the heterogeneous stress fields. The average value of the estimated differential stresses in the region was 15.4 +/- 10 MPa. The rotation of the principal stress axes and the low differential stress are important information to understand the physical processes of the earthquake generation and the state of the crustal stress.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 125, 号 9, 発行日 2020-09
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 2169-9356
DOI
関連識別子 10.1029/2019JB018515
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