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微動アレイ観測に基づく福井平野の深部地盤速度構造の照査・検討
https://doi.org/10.57375/00000280
https://doi.org/10.57375/000002800b90399c-fae3-45a6-85f0-cc880413adca
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-03-23 | |||||
タイトル | ||||||
タイトル | 微動アレイ観測に基づく福井平野の深部地盤速度構造の照査・検討 | |||||
タイトル | ||||||
タイトル | Examination on Deep Soil Velocity Structure of Fukui Plain Through Microtremor Array Observation | |||||
言語 | en | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.57375/00000280 | |||||
ID登録タイプ | JaLC | |||||
著者 |
安井, 譲
× 安井, 譲× 森本, 鉄郎× 野口, 竜也× Yasui, Yuzuru× Morimoto, Tetsuro× Noguchi, Tatsuya |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | "In Fukui plain, Fukui Ddoboku Jimusho is the only point where deep soil profile down to tertiary layer is obtained by direct method such as PS logging test. There are three soil velocity models about Fukui plain. One is Fukui prefecture model that is made from shallow boring data referring the Fukui Doboku Jimusho point soil profile. Another model is microtremor model being made through microtremor observation method. The other one is gravity model obtained through gravitational survey method. However, there are big difference between those three models on depth of tertiary layer or seismic bedrock. And so we conducted microtremor array observation at some typical points useful to examination on the deep soil profile of the three models and discussed the obtained results." | |||||
書誌情報 |
福井工業大学研究紀要. 第一部 号 38, p. 199-206, 発行日 2008-05-31 |
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出版者 | ||||||
出版者 | 福井工業大学 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 2868571 | |||||
書誌レコードID | ||||||
識別子タイプ | NCID | |||||
関連識別子 | TF00008739 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |