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  1. 防災科研関係論文

Shallow magmatic hydrothermal eruption in April 2018 on Ebinokogen-Ioyama volcano in Kirishima volcano group, Kyushu, Japan

https://nied-repo.bosai.go.jp/records/5771
https://nied-repo.bosai.go.jp/records/5771
41f86a06-2674-4df1-b086-aa5bf2ea5575
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Shallow magmatic hydrothermal eruption in April 2018 on Ebinokogen-Ioyama volcano in Kirishima volcano group, Kyushu, Japan
著者 Yasuhisa Tajima

× Yasuhisa Tajima

en Yasuhisa Tajima

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Setsuya Nakada

× Setsuya Nakada

en Setsuya Nakada

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Fukashi Maeno

× Fukashi Maeno

en Fukashi Maeno

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Toshio Huruzono

× Toshio Huruzono

en Toshio Huruzono

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Masaaki Takahashi

× Masaaki Takahashi

en Masaaki Takahashi

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Akihiko Inamura

× Akihiko Inamura

en Akihiko Inamura

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Takeshi Matsushima

× Takeshi Matsushima

en Takeshi Matsushima

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Masashi Nagai

× Masashi Nagai

en Masashi Nagai

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Jun Funasaki

× Jun Funasaki

en Jun Funasaki

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抄録
内容記述タイプ Other
内容記述 c 2020 by the authors. Licensee MDPI, Basel, Switzerland. The Kirishima Volcano Group is a volcanic field ideal for studying the mechanism of steam-driven eruptions because many eruptions of this type occurred in the historical era and geophysical observation networks have been installed in this volcano. We made regular geothermal observations to understand the hydrothermal activity in Ebinokogen Ioyama Volcano. Geothermal activity resumed around the Ioyama from December 2015. A steam blowout occurred in April 2017, and a hydrothermal eruption occurred in April 2018. Geothermal activity had gradually increased before these events, suggesting intrusion of the magmatic component fluids in the hydrothermal system under the volcano. The April 2018 eruption was a magmatic hydrothermal eruption caused by the injection of magmatic fluids into a very-shallow hydrothermal system as a bottom?up fluid pressurization, although juvenile materials were not identifiable. Additionally, the upwelling of mixed magma?meteoric fluids to the surface as a kick was observed just before the eruption to cause the top?down flashing of April 2018. A series of events was generated in the shallower hydrothermal regime consisting of multiple systems divided by conductive caprock layers.
言語 en
書誌情報 en : Geosciences (Switzerland)

巻 10, 号 5, p. 32-55, 発行日 2020-05
ISSN
収録物識別子タイプ EISSN
収録物識別子 2076-3263
DOI
関連識別子 10.3390/geosciences10050183
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