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変動地形からみた相模トラフにおけるプレート間地震サイクル
https://doi.org/10.15083/0000032554
https://doi.org/10.15083/00000325543ae535f4-00af-4034-b31b-bbe8edef8b0f
名前 / ファイル | ライセンス | アクション |
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IHO78303.pdf (6.5MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2007-04-23 | |||||
タイトル | ||||||
タイトル | 変動地形からみた相模トラフにおけるプレート間地震サイクル | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | tectonic geomorphology | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | paleo-shoreline | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | recurrence interval | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Sagami Trough | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Kanto Earthquake | |||||
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 | 10.15083/0000032554 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Cycle of Interplate Earthquake Along the Sagami Trough, Deduced from Tectonic Geomorphology | |||||
著者 |
宍倉, 正展
× 宍倉, 正展 |
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著者別名 | ||||||
識別子 | 125583 | |||||
識別子Scheme | WEKO | |||||
姓名 | Shishikura, Masanobu | |||||
著者所属 | ||||||
著者所属 | 産業技術総合研究所活断層研究センター | |||||
著者所属 | ||||||
著者所属 | Active Fault Reserch Center, GSJ/AIST | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | A tectonic geomorphological study is one of the best methods of evaluating the timing and the crustal deformation of pre-historic earthquake. To reveal the cycle of interplate earthquakes along the Sagami Trough, I investigatedthe emergedshoreline topography andthe fossilizedsessile assemblages in the Miura Peninsula andthe Boso Peninsula. The distribution pattern of coseismic vertical displacement during the 1703 Genroku Kanto Earthquake inferredfrom the height distribution of the paleo-shoreline suggests that the fault source model consists of a dual fault system of the Fault A andB. Fault A is also the source of the 1923 Taisho Kanto Earthquake. The geometry and ages of the emerged shoreline topography divided into several levels indicate that the characteristic earthquake generatedfrom Fault A has occurredabout every 400 years. One of several events, it is accompaniedwith a slip of Fault B, which has a recurrence interval of 2000-2700 years. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 78, 号 3, p. 245-254, 発行日 2003 |
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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 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |