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  1. 防災科研関係論文

Inversion Analysis for Horizontal-to-Vertical Spectral Ratio of Earthquake at S-net Sites Focusing on Relatively Low Frequency Range

https://nied-repo.bosai.go.jp/records/7322
https://nied-repo.bosai.go.jp/records/7322
03e94024-5e2e-454d-adce-9a21b51111f6
Item type researchmap(1)
公開日 2025-10-06
タイトル
言語 en
タイトル Inversion Analysis for Horizontal-to-Vertical Spectral Ratio of Earthquake at S-net Sites Focusing on Relatively Low Frequency Range
言語
言語 eng
著者 Fumiaki Nagashima

× Fumiaki Nagashima

en Fumiaki Nagashima

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Yadab P. Dhakal

× Yadab P. Dhakal

en Yadab P. Dhakal

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Hiroshi Kawase

× Hiroshi Kawase

en Hiroshi Kawase

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Kenichi Nakano

× Kenichi Nakano

en Kenichi Nakano

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Takashi Kunugi

× Takashi Kunugi

en Takashi Kunugi

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抄録
内容記述タイプ Other
内容記述 Since underground structures in the sea area are difficult to observe, they are not well examined. To estimate underground structures beneath Seafloor Observation Network for Earthquakes and Tsunamis along the Japan Trench (S-net), which was installed in the sea area between the Japanese islands and the outer rise of the Japan Trench, horizontal-to-vertical spectral ratios of earthquake motions (EHVRs) recorded at S-net sites were calculated, and the EHVRs were inverted to obtain one-dimensional seismic velocity structures. The effect of reflected waves from sea surface was not found on the observed EHVRs; however, the sharp trough and directional dependency, possibly owing to the seismometers’ installing situation, were found on the observed EHVRs. Inversion analysis of the observed EHVRs based on the diffuse field concept for earthquake was performed within 0.1–3.0 Hz avoiding the sharp trough and the directional dependency. The observed EHVRs were well reproduced by the resultant seismic velocity structures. The travel times for S- and P-waves from the seismic bedrock (S-wave velocity =3100 m/s) to the seafloor were calculated from the identified structures, and it was distributed between 2.8 s and 3.8 s for S-wave velocity and 0.9 s and 1.3 s for P-wave velocity. Comparing the identified structures with previous studies revealed similar depths to seismic bedrock; however, some discrepancies were noted. Such correspondences and discrepancies exhibit the validity and limitation of our inversion models. The possible causes of discrepancies are the difference of the observed data, the target frequency range, and the inversion conditions. Therefore, in the future, more detailed investigations should be performed.
言語 en
書誌情報 en : Journal of Disaster Research

巻 20, 号 5, p. 628-638, 発行日 2025-10-01
出版者
言語 en
出版者 Fuji Technology Press Ltd.
ISSN
収録物識別子タイプ EISSN
収録物識別子 1883-8030
DOI
関連識別子 10.20965/jdr.2025.p0628
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