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2007年能登半島地震震源域陸域の反射法地震探査
https://doi.org/10.15083/0000032466
https://doi.org/10.15083/000003246657342e73-b649-4f4a-8e3d-f67dfcd27ddf
名前 / ファイル | ライセンス | アクション |
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IHO82404.pdf (1.4MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-07-15 | |||||
タイトル | ||||||
タイトル | 2007年能登半島地震震源域陸域の反射法地震探査 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | 2007 Noto Hanto earthquake | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | earthquake source fault | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | seismic reflection profiling | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | geo-logic structure, central Japan | |||||
主題Scheme | Other | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000032466 | |||||
ID登録タイプ | JaLC | |||||
著者 |
佐藤, 比呂志
× 佐藤, 比呂志× 川崎, 慎治× 阿部, 進× 加藤, 直子× 岩崎, 貴哉× 伊藤, 谷生 |
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著者別名 | ||||||
識別子 | 123963 | |||||
識別子Scheme | WEKO | |||||
姓名 | Sato, Hiroshi | |||||
著者別名 | ||||||
識別子 | 123964 | |||||
識別子Scheme | WEKO | |||||
姓名 | Kawasaki, Shinji | |||||
著者別名 | ||||||
識別子 | 123965 | |||||
識別子Scheme | WEKO | |||||
姓名 | Abe, Susumu | |||||
著者別名 | ||||||
識別子 | 123966 | |||||
識別子Scheme | WEKO | |||||
姓名 | Kato, Naoko | |||||
著者別名 | ||||||
識別子 | 123967 | |||||
識別子Scheme | WEKO | |||||
姓名 | Iwasaki, Takaya | |||||
著者別名 | ||||||
識別子 | 123968 | |||||
識別子Scheme | WEKO | |||||
姓名 | Ito, Tanio | |||||
著者所属 | ||||||
著者所属 | 東京大学地震研究所 | |||||
著者所属 | ||||||
著者所属 | (株)地球科学総合研究所 | |||||
著者所属 | ||||||
著者所属 | 千葉大学大学院理学研究科 | |||||
著者所属 | ||||||
著者所属 | Earthquake Research Institute, the University of Tokyo | |||||
著者所属 | ||||||
著者所属 | JGI Inc. | |||||
著者所属 | ||||||
著者所属 | Graduate School of Science, Chiba University | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The seismogenic source fault of the 2007 Noto Hanto earthquake (M 6.9JMA) runs beneath the northwestern part of the Noto peninsula and its offshore trending ENE-WSW. To reveal the rela-tionship between a seismogenic source fault and geologic structure, shallow, high-resolution seismic reflection and refraction profiling was undertaken across the source fault along the western coast of the Noto peninsula for 10km distance. The seismic source was a vibroseis and seismic data were recorded by fixed 575 channels. The P-wave refraction analysis delineated the three layered velocity structure down to 1km; 2.8km/s, 3.2km/s and 4.1km/s layers. The 3.2km/s layer, which corresponds to the lower Miocene fluvial sediments, shows northward thickening with steps. On the resultant depth converted seismic section, south and north-dipping, faults are interpreted based on the systematic change on dip-angle of the reflectors in the lower Miocene fluvial sediments. By comparing with the aftershock distribution, the deeper extension of the south-dipping fault corresponds to the source fault of the 2007 Noto Hanto earthquake. | |||||
書誌情報 |
地震研究所彙報 巻 82, 号 4, p. 265-273, 発行日 2007 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 51.1 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |