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  1. 防災科研関係論文

Modeling of Long-Period Ground Motions in the Nankai Subduction Zone: Model Simulation Using the Accretionary Prism Derived from Oceanfloor Local S-Wave Velocity Structures

https://nied-repo.bosai.go.jp/records/4140
https://nied-repo.bosai.go.jp/records/4140
662f3964-a871-4dec-8a0b-a42357fbd6df
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Modeling of Long-Period Ground Motions in the Nankai Subduction Zone: Model Simulation Using the Accretionary Prism Derived from Oceanfloor Local S-Wave Velocity Structures
言語
言語 eng
著者 Shunsuke Takemura

× Shunsuke Takemura

en Shunsuke Takemura

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Hisahiko Kubo

× Hisahiko Kubo

en Hisahiko Kubo

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Takashi Tonegawa

× Takashi Tonegawa

en Takashi Tonegawa

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Tatsuhiko Saito

× Tatsuhiko Saito

en Tatsuhiko Saito

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Katsuhiko Shiomi

× Katsuhiko Shiomi

en Katsuhiko Shiomi

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抄録
内容記述タイプ Other
内容記述 The accretionary prism in the subduction zone, which consists of thick low-velocity oceanic sediments, significantly affects the propagation of seismic waves for shallow, offshore earthquakes, including large interplate earthquakes. In order to simulate long-period (>5s) ground motions in the Nankai subduction zone, we constructed a three-dimensional (3D) seismic velocity structure model of the accretionary prism by interpolation/extrapolation of local S-wave velocity structures beneath 46 oceanfloor seismic stations (DONET), which are deployed just above the accretionary prism off the southern Kii and eastern Shikoku regions. We modeled local S-wave velocity structures using a simple two-parameter depth-varying velocity function. To investigate the effects of the accretionary prism on ground and seafloor motions, we conducted numerical simulations of seismic wave propagation for three local earthquakes that occurred in southwestern Japan. The simulations reasonably reproduced the observed seismograms, not only for the period ranges of the moment tensor inversion (similar to 50s), but also for the strong, long-period ground motions in the sedimentary basins (similar to 5s), especially in the region where DONET stations are densely deployed. Since depth-varying, local S-wave structures significantly improve the reproducibility of long-period ground motions, our modeling procedure is useful for modeling long-period ground motions of local and regional offshore subduction zone earthquakes.
言語 en
書誌情報 en : Pure and Applied Geophysics

巻 176, 号 2, p. 627-647
出版者
言語 en
出版者 Springer Science and Business Media LLC
ISSN
収録物識別子タイプ EISSN
収録物識別子 1420-9136
DOI
関連識別子 10.1007/s00024-018-2013-8
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