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  1. 防災科研関係論文

Precise Monitoring of Pore Pressure at Boreholes Around Nankai Trough Toward Early Detecting Crustal Deformation

https://nied-repo.bosai.go.jp/records/5765
https://nied-repo.bosai.go.jp/records/5765
568d31a4-c059-4bf1-b8fc-82cf9cad903a
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Precise Monitoring of Pore Pressure at Boreholes Around Nankai Trough Toward Early Detecting Crustal Deformation
著者 Keisuke Ariyoshi

× Keisuke Ariyoshi

en Keisuke Ariyoshi

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Toshinori Kimura

× Toshinori Kimura

en Toshinori Kimura

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Yasumasa Miyazawa

× Yasumasa Miyazawa

en Yasumasa Miyazawa

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Sergey Varlamov

× Sergey Varlamov

en Sergey Varlamov

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Takeshi Iinuma

× Takeshi Iinuma

en Takeshi Iinuma

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Akira Nagano

× Akira Nagano

en Akira Nagano

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Joan Gomberg

× Joan Gomberg

en Joan Gomberg

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Eiichiro Araki

× Eiichiro Araki

en Eiichiro Araki

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Toru Miyama

× Toru Miyama

en Toru Miyama

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Kentaro Sueki

× Kentaro Sueki

en Kentaro Sueki

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Shuichiro Yada

× Shuichiro Yada

en Shuichiro Yada

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Takane Hori

× Takane Hori

en Takane Hori

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Narumi Takahashi

× Narumi Takahashi

en Narumi Takahashi

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Shuichi Kodaira

× Shuichi Kodaira

en Shuichi Kodaira

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抄録
内容記述タイプ Other
内容記述 In our recent study, we detected the pore pressure change due to the slow slip event (SSE) in March 2020 at the two borehole stations (C0002 and C0010), where the other borehole (C0006) close to the Nankai Trough seems not because of instrumental drift for the reference pressure on the seafloor to remove non-crustal deformation such as tidal and oceanic fluctuations. To overcome this problem, we use the seafloor pressure gauges of cabled network Dense Oceanfloor Network System for Earthquakes and Tsunamis (DONET) stations nearby boreholes instead of the reference by introducing time lag between them. We confirm that the time lag is explained from superposition of theoretical tide modes. By applying this method to the pore pressure during the SSE, we find pore pressure change at C0006 about 0.6?hPa. We also investigate the impact of seafloor pressure due to ocean fluctuation on the basis of ocean modeling, which suggests that the decrease of effective normal stress from the onset to the termination of the SSE is explained by Kuroshio meander and may promote updip slip migration, and that the increase of effective normal stress for the short-term ocean fluctuation may terminate the SSE as observed in the Hikurangi subduction zone.
言語 en
書誌情報 en : Frontiers in Earth Science

巻 9, 発行日 2021-08-27
出版者
言語 en
出版者 Frontiers Media SA
ISSN
収録物識別子タイプ EISSN
収録物識別子 2296-6463
DOI
関連識別子 10.3389/feart.2021.717696
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