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  1. 防災科研関係論文

Waveform Inversion による盆地構造の境界面形状の推定

https://nied-repo.bosai.go.jp/records/5849
https://nied-repo.bosai.go.jp/records/5849
d5152b6f-aaca-44ad-8a64-99be464b6ead
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Waveform Inversion による盆地構造の境界面形状の推定
タイトル
言語 en
タイトル Waveform Inversion for the Boundary Shape of Basin Structures
著者 青井 真

× 青井 真

ja 青井 真

en AOI Shin

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岩田 知孝

× 岩田 知孝

ja 岩田 知孝

en IWATA Tomotaka

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小林 芳正

× 小林 芳正

ja 小林 芳正

en KOBAYASHI Yoshimasa

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入倉 孝次郎

× 入倉 孝次郎

ja 入倉 孝次郎

en IRIKURA Kojiro

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抄録
内容記述タイプ Other
内容記述 We develop a method to determine the boundary shape of basin structures using seismograms observed on the surface through a waveform inversion scheme. Our method is based on the fact that seismic waves observed at stations on the surface are affected not only by the local structure beneath the observation point but also by the whole basin structure. This fact suggests a possibility to determine the boundary shape by using the seismic records at only a few surface stations. This paper examines numerically how to determine the boundary shape from observed records on the surface in the case of the two dimensional SH problem. For simplicity, we parameterize only the boundary shape, i. e. the thickness variation of the sedimental layer. This inversion is performed iteratively since the problem we deal with is a non-linear inverse problem. When an appropriate model is given, we can evaluate the boundary shape accurately even though the waveform data at only a few surface stations are given.
言語 ja
抄録
内容記述タイプ Other
内容記述 We develop a method to determine the boundary shape of basin structures using seismograms observed on the surface through a waveform inversion scheme. Our method is based on the fact that seismic waves observed at stations on the surface are affected not only by the local structure beneath the observation point but also by the whole basin structure. This fact suggests a possibility to determine the boundary shape by using the seismic records at only a few surface stations. This paper examines numerically how to determine the boundary shape from observed records on the surface in the case of the two dimensional SH problem. For simplicity, we parameterize only the boundary shape, i. e. the thickness variation of the sedimental layer. This inversion is performed iteratively since the problem we deal with is a non-linear inverse problem. When an appropriate model is given, we can evaluate the boundary shape accurately even though the waveform data at only a few surface stations are given.
言語 en
書誌情報 ja : 地震 第2輯
en : Zisin (Journal of the Seismological Society of Japan. 2nd ser.)

巻 46, 号 2, p. 95-107, 発行日 1993
出版者
言語 ja
出版者 公益社団法人 日本地震学会
出版者
言語 en
出版者 SEISMOLOGICAL SOCIETY OF JAPAN
ISSN
収録物識別子タイプ ISSN
収録物識別子 0037-1114
DOI
関連識別子 10.4294/zisin1948.46.2_95
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