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  1. 防災科研関係論文

Gas pathways and remotely triggered earthquakes beneath Mount Fuji, Japan

https://nied-repo.bosai.go.jp/records/4845
https://nied-repo.bosai.go.jp/records/4845
fbb95dec-965c-4dbd-8add-5a6bd10a876f
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Gas pathways and remotely triggered earthquakes beneath Mount Fuji, Japan
言語
言語 eng
著者 Koki Aizawa

× Koki Aizawa

en Koki Aizawa

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Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

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Makoto Uyeshima

× Makoto Uyeshima

en Makoto Uyeshima

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Yusuke Yamaya

× Yusuke Yamaya

en Yusuke Yamaya

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Hideaki Hase

× Hideaki Hase

en Hideaki Hase

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Hiroshi A. Takahashi

× Hiroshi A. Takahashi

en Hiroshi A. Takahashi

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Masaaki Takahashi

× Masaaki Takahashi

en Masaaki Takahashi

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Kohei Kazahaya

× Kohei Kazahaya

en Kohei Kazahaya

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Masao Ohno

× Masao Ohno

en Masao Ohno

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Tawat Rung-Arunwan

× Tawat Rung-Arunwan

en Tawat Rung-Arunwan

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Yasuo Ogawa

× Yasuo Ogawa

en Yasuo Ogawa

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抄録
内容記述タイプ Other
内容記述 Large earthquakes sometimes trigger local seismicity that is distal to their rupture zones. Various mechanisms for this triggered seismicity have been proposed, based on either the static stress change or ground shaking from seismic waves, but local geological structure is rarely studied to discern why this seismicity is remotely induced. We present the results of a joint three-dimensional resistivity and isotopic analysis of the groundwater system surrounding Mount Fuji, Japan, where increased seismicity was observed following the A.D. 2011 Tohoku-Oki megathrust earthquake. An electrically conductive zone and high concentrations of magmatic gases (He and CO2) correspond to the zone of triggered seismicity. In contrast, a contribution of magmatic water is not suggested from H-2 (deuterium, D) and O-18 isotope ratios. These results suggest that the earthquakes were triggered within a fractured zone through which magmatic gases preferentially migrated. We hypothesize that the upwelling of gas-rich hydrous fluids and/or gas bubbles occurred along this fracture pathway, causing an increase in the pore pressure and triggering the resultant earthquake sequence.
言語 en
書誌情報 en : GEOLOGY

巻 44, 号 2, p. 127-130, 発行日 2016-02
出版者
言語 en
出版者 GEOLOGICAL SOC AMER, INC
ISSN
収録物識別子タイプ EISSN
収録物識別子 1943-2682
DOI
関連識別子 10.1130/G37313.1
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