WEKO3
アイテム
2007年能登半島地震の海底地殻変動
https://doi.org/10.15083/0000032471
https://doi.org/10.15083/0000032471647240c8-97a4-45b1-8556-daf7ba013b8b
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
IHO82409.pdf (1.6MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-07-15 | |||||
| タイトル | ||||||
| タイトル | 2007年能登半島地震の海底地殻変動 | |||||
| 言語 | ja | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | the 2007 Noto Hanto Earthquake | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | offshore crustal movement | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | echo sounding | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | sonic prospecting | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | recurrence interval | |||||
| 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 | 10.15083/0000032471 | |||||
| ID登録タイプ | JaLC | |||||
| 著者 |
吉田, 進
× 吉田, 進× 野口, 猛雄× 長, 貴浩× 島崎, 裕行× 木場, 正信× 佐藤, 比呂志 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124021 | |||||
| 姓名 | Yoshida, Susumu | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124022 | |||||
| 姓名 | Noguchi, Takeo | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124023 | |||||
| 姓名 | Cho, Takahiro | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124024 | |||||
| 姓名 | Shimazaki, Masanori | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124025 | |||||
| 姓名 | Koba, Masanobu | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 124026 | |||||
| 姓名 | Sato, Hiroshi | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The 2007 Noto Hanto earthquake produced flexure along the known active fault in the offshore focal area. To reveal the amount of vertical crustal movement, echo sounding and sonic prospecting were carried out just after the earthquake. The new observations were carefully compared to the previous data acquired in 1985 and 2006 and co-seismic vertical crustal movement was obtained along several tracks. The upheaval zone was observed along the hanging wall of the active fault at 1－3km. A 2m maximum upheaval was found in the northeastern part of the fault trace. Together with the source fault geometry obtained by the seismic reflection profiling and aftershock distribution, the slip distribution on the fault plane obtained by two-dimension section was calculated us-ing the vertical displacement in the focal area, suggesting that a larger slip was estimated in the shallower part of the fault surface. Based on the vertical displacement of the erosion surface formed at the last glacial age and the newly obtained co-seismic displacement of the 2007 earthquake, the average recurrence interval is estimated to be 1700 (1300－2000) years. | |||||
| 書誌情報 |
地震研究所彙報 巻 82, 号 4, p. 333-344, 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Scheme | NDC | |||||
| 主題 | 51.1 | |||||
| 出版者 | ||||||
| 出版者 | 地震研究所 | |||||
| 出版者別名 | ||||||
| Earthquake Research Institute, University of Tokyo | ||||||
