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  1. 防災科研関係論文

Source parameters of the 2007 Noto Hanto earthquake sequence derived from strong motion records at temporary and permanent stations

https://nied-repo.bosai.go.jp/records/5018
https://nied-repo.bosai.go.jp/records/5018
62281f91-a24f-403a-81eb-f26f3ee7a72e
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Source parameters of the 2007 Noto Hanto earthquake sequence derived from strong motion records at temporary and permanent stations
言語
言語 eng
著者 Takahiro Maeda

× Takahiro Maeda

en Takahiro Maeda

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Masayoshi Ichiyanagi

× Masayoshi Ichiyanagi

en Masayoshi Ichiyanagi

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Hiroaki Takahashi

× Hiroaki Takahashi

en Hiroaki Takahashi

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Ryo Hondo

× Ryo Hondo

en Ryo Hondo

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Teruhiro Yamaguchi

× Teruhiro Yamaguchi

en Teruhiro Yamaguchi

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Minoru Kasahara

× Minoru Kasahara

en Minoru Kasahara

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Tsutomu Sasatani

× Tsutomu Sasatani

en Tsutomu Sasatani

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抄録
内容記述タイプ Other
内容記述 A large crustal earthquake, the 2007 Nolo Hanto earthquake, occurred west off the Noto peninsula in Ishikawa prefecture. Japan, oil March 25, 2007. We started temporary strong motion observation Lit live sites within the aftershock area from about 13 h after the main shock occurrence. We first applied file spectral inversion method to S-wave strong ground motion records at the temporary and permanent stations. We obtained source specta of the main shock and aftershocks, Q(s) (quality factor for S-wave) values (Q(s) = 34.5f(0.95)) and site responses at 22 sites. We then estimated a source model of the main shock using the empirical Green's function method. The source model Consists Of three strong motion generation areas and well explains the observed records. Finally, we examined the consistency of the main-shock SOLH-CC models estimated from the above two analyses. The high-frequency level of the acceleration source spectrum based on the main-shock source model is consistent With the source spectrum estimated from the spectral inversion. The combined area of strong motion generation areas is approximately half of the value expected by the empirical relationship, and the high-frequency level of acceleration source spectrum is approximately 2.5 times larger than the empirical relationship for shallow inland and inter-plate earthquakes.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 60, 号 10, p. 1011-1016
出版者
言語 en
出版者 TERRA SCIENTIFIC PUBL CO
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.1186/BF03352861
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