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Transient uplift after a 17th-century earthquake along the kuril subduction zone
https://ir.soken.ac.jp/records/3943
https://ir.soken.ac.jp/records/3943e35b0888-3b61-4986-ba64-a2d131a61fb9
Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2013-08-29 | |||||
タイトル | ||||||
タイトル | Transient uplift after a 17th-century earthquake along the kuril subduction zone | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Transient uplift after a 17th-century earthquake along the kuril subduction zone | |||||
言語 | ||||||
言語 | eng | |||||
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 | journal article | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
著者 |
SAWAI, Yuki
× SAWAI, Yuki× SATAKE, Kenji× KAMATAKI, Takanobu× NASU, Hiroo× et, al. |
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著者別名 |
那須, 浩郎
× 那須, 浩郎 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | In eastern Hokkaido, 60 to 80 kilometers above a subducting oceanic plate, tidal mudflats changed into freshwater forests during the first decades after a 17th-century tsunami. The mudflats gradually rose by a meter, as judged from fossil diatom assemblages. Both the tsunami and the ensuing uplift exceeded any in the region's 200 years of written history, and both resulted from a shallow plate-boundary earthquake of unusually large size along the Kuril subduction zone. This earthquake probably induced more creep farther down the plate boundary than did any of the region's historical events. | |||||
書誌情報 |
Science en : Science 巻 306, 号 5703, p. 1918-1920, 発行日 2004-12-10 |
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出版者 | ||||||
出版者 | American Association for the Advancement of Science | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00368075 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | http://doi.org/10.1126/science.1104895 | |||||
関連名称 | 10.1126/science.1104895 | |||||
権利 | ||||||
権利情報 | © American Association for the Advancement of Science |