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  1. 防災科研関係論文

<i>S</i>-wave modelling of the Showa-Shinzan lava dome in Usu Volcano, Northern Japan, from seismic observations

https://nied-repo.bosai.go.jp/records/2930
https://nied-repo.bosai.go.jp/records/2930
ccc7f369-76da-43e6-a38e-06fcbbfdec42
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル <i>S</i>-wave modelling of the Showa-Shinzan lava dome in Usu Volcano, Northern Japan, from seismic observations
言語
言語 eng
著者 Akiko Takeo

× Akiko Takeo

en Akiko Takeo

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Kiwamu Nishida

× Kiwamu Nishida

en Kiwamu Nishida

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Hiroshi Aoyama

× Hiroshi Aoyama

en Hiroshi Aoyama

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Motoko Ishise

× Motoko Ishise

en Motoko Ishise

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Takeru Kai

× Takeru Kai

en Takeru Kai

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Ryo Kurihara

× Ryo Kurihara

en Ryo Kurihara

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Takuto Maeda

× Takuto Maeda

en Takuto Maeda

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Yuta Mizutani

× Yuta Mizutani

en Yuta Mizutani

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Yuki Nakashima

× Yuki Nakashima

en Yuki Nakashima

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Shogo Nagahara

× Shogo Nagahara

en Shogo Nagahara

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Xiaowen Wang

× Xiaowen Wang

en Xiaowen Wang

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Lingling Ye

× Lingling Ye

en Lingling Ye

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Takeshi Akuhara

× Takeshi Akuhara

en Takeshi Akuhara

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Yosuke Aoki

× Yosuke Aoki

en Yosuke Aoki

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抄録
内容記述タイプ Other
内容記述 SUMMARY

To obtain an internal S-wave velocity structure, we conducted a passive seismic campaign with 21 1-Hz seismometers on and around the Showa-Shinzan lava dome, which emerged during the 1943?1945 eruption of Usu Volcano, Japan. Before the campaign, we calibrated seismometers and found slight phase-response differences between seismometers of less than 1?2°. After the campaign, we extracted seismic wavefield by taking cross-correlations of vertical-component ambient noise records between seismic sites. We developed a new method to measure phase velocities of the Rayleigh wave automatically by assuming layered structure and finally obtained 1-D S-wave velocity models in summit, roof and base regions. The obtained S-wave velocity right beneath the intruded lava dome is higher than that in surrounding areas by a few tens of per cent down to a few hundred metres below sea level, indicating narrow but deep existence of the root of the lava dome. The obtained S-wave velocity at depths shallower than ?50?m inside the lava dome in the summit area was ?1?km?s?1, significantly lower than that predicted from the density of ?2.3 × 103?kg?m?3 estimated in previous muon-radiography studies and a conventional scaling, indicating the effect of cracking in the lava dome.
言語 en
書誌情報 en : Geophysical Journal International

巻 230, 号 3, p. 1662-1678, 発行日 2022-05-19
出版者
言語 en
出版者 Oxford University Press (OUP)
ISSN
収録物識別子タイプ EISSN
収録物識別子 1365-246X
DOI
関連識別子 10.1093/gji/ggac111
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