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  1. 防災科研関係論文

孔内観測とDONETから捉えられた2020年3月の熊野灘スロースリップイベントに対する黒潮蛇行の影響に関する考察

https://nied-repo.bosai.go.jp/records/3342
https://nied-repo.bosai.go.jp/records/3342
2f8ff9e6-1798-4980-b809-4b9a56f46736
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 ja
タイトル 孔内観測とDONETから捉えられた2020年3月の熊野灘スロースリップイベントに対する黒潮蛇行の影響に関する考察
タイトル
言語 en
タイトル (entry) Impact of Kuroshio meander on the slow slip event in March 2020 detected by borehole and DONET observatories
言語
言語 jpn
著者 有吉 慶介

× 有吉 慶介

ja 有吉 慶介

en Ariyoshi Keisuke

Search repository
木村 俊則

× 木村 俊則

ja 木村 俊則

en Kimura Toshinori

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宮澤 泰正

× 宮澤 泰正

ja 宮澤 泰正

en Miyazawa Yasumasa

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バーラモフ セルゲイ

× バーラモフ セルゲイ

ja バーラモフ セルゲイ

en Sergey Varlamov

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飯沼 卓史

× 飯沼 卓史

ja 飯沼 卓史

en Iinuma Takeshi

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永野 憲

× 永野 憲

ja 永野 憲

en Nagano Akira

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ゴンバーグ ジョアン

× ゴンバーグ ジョアン

ja ゴンバーグ ジョアン

en Gomberg Joan

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荒木 英一郎

× 荒木 英一郎

ja 荒木 英一郎

en Araki Eiichiro

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美山 透

× 美山 透

ja 美山 透

en Miyama Toru

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末木 健太郎

× 末木 健太郎

ja 末木 健太郎

en Sueki Kentaro

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矢田 修一郎

× 矢田 修一郎

ja 矢田 修一郎

en Yada Shuichiro

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堀 高峰

× 堀 高峰

ja 堀 高峰

en Hori Takane

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高橋 成実

× 高橋 成実

ja 高橋 成実

en Takahashi Narumi

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小平 秀一

× 小平 秀一

ja 小平 秀一

en Kodaira Shuichi

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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 (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 ja
書誌情報 ja : 日本地質学会学術大会講演要旨
en : Annual Meeting of the Geological Society of Japan

巻 2021, p. 184, 発行日 2021
出版者
言語 ja
出版者 一般社団法人 日本地質学会
出版者
言語 en
出版者 The Geological Society of Japan
ISSN
収録物識別子タイプ EISSN
収録物識別子 2187-6665
DOI
関連識別子 10.14863/geosocabst.2021.0_184
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