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常時微動観測に基づく敦賀平野のS波速度構造の推定
http://hdl.handle.net/10098/2173
http://hdl.handle.net/10098/21738f680f5d-898b-4323-b325-404f1ba53651
名前 / ファイル | ライセンス | アクション |
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BD00006820_001.pdf (1.4 MB)
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日本自然災害学会
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2009-10-26 | |||||
タイトル | ||||||
タイトル | 常時微動観測に基づく敦賀平野のS波速度構造の推定 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Estimation of S-wave Velocity Structure of Tsuruga Plain Based on Microtremor Observation | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 敦賀平野 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 常時微動観測 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 位相速度 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | H/Vスぺクトル | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | S波速度構造 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Tsuruga Plain | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | microtremor observation | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | phase velocity | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | H/V-spectrum | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | S-wave velocity structure | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_1843 | |||||
資源タイプ | other | |||||
著者 |
小嶋, 啓介
× 小嶋, 啓介× 野口, 竜也× 佐藤, 毅× 黒田, 貴紀× KOJIMA, Keisuke× NOGUCHI, Tatsuya× SATHO, Takeshi× KURODA, Takanori |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The accurate estimations of Quaternary structure are indispensable in order to accurately predict the seismic damage of the region. However, around the Tsuruga Plain, subsurface investigation infonnation such as the S-wave velocity structure hardly exists. The problems analyzed in this study are estimations of 3D Quaternary configuration of the Tsuruga Plain using the data from microtremor observations. Microtremor array observations have been conducted at twelve sites in order to determine the S-wave velocity structure. The phase velocities at each site were inverted to a vertical S-wave profile using a genetic algorithm. To interpolate the array observations, the 3-components microtremor observations were carried out at 58 points. The 3D configuration models of Quaternary have been evaluated by using geo-statistical procedure. By comparing with the inverted structure of gravity anomaly observation and with the existing data, the validity of the estimated structure was examined. | |||||
書誌情報 |
自然災害科学 巻 27, 号 1, p. 85-96, 発行日 2008-05-31 |
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出版者 | ||||||
出版者 | 日本自然災害学会 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 2866021 | |||||
書誌レコードID | ||||||
識別子タイプ | NCID | |||||
関連識別子 | TD00006820 | |||||
著者版フラグ | ||||||
出版タイプ | AO | |||||
出版タイプResource | http://purl.org/coar/version/c_b1a7d7d4d402bcce |