| Item type |
学術雑誌論文 / Journal Article(1) |
| 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 |
|
|
タイトル |
Transient uplift after a 17th-century earthquake along the kuril subduction zone |
|
言語 |
en |
| 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
SATAKE, Kenji
KAMATAKI, Takanobu
NASU, Hiroo
et, al.
|
| 著者別名 |
那須, 浩郎
|
| 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
|
| 出版者 |
|
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出版者 |
American Association for the Advancement of Science |
| ISSN |
|
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収録物識別子タイプ |
ISSN |
|
収録物識別子 |
00368075 |
| DOI |
|
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|
識別子タイプ |
DOI |
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関連識別子 |
http://doi.org/10.1126/science.1104895 |
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関連名称 |
10.1126/science.1104895 |
| 権利 |
|
|
権利情報 |
© American Association for the Advancement of Science |
