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  1. 010 学術雑誌論文
  2. 那須, 浩郎 / NASU, Hiroo

Aperiodic recurrence of geologically recorded tsunamis during the past 5500 years in eastern Hokkaido, Japan

https://ir.soken.ac.jp/records/3938
https://ir.soken.ac.jp/records/3938
fd263af1-a047-4d65-a3a2-928a68f3fcad
Item type 学術雑誌論文 / Journal Article(1)
公開日 2013-08-28
タイトル
タイトル Aperiodic recurrence of geologically recorded tsunamis during the past 5500 years in eastern Hokkaido, Japan
タイトル
タイトル Aperiodic recurrence of geologically recorded tsunamis during the past 5500 years in eastern Hokkaido, Japan
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

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SAWAI, Yuki

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KAMATAKI, Takanobu

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KAMATAKI, Takanobu

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SHISHIKURA, Masanobu

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SHISHIKURA, Masanobu

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NASU, Hiroo

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NASU, Hiroo

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et, al.

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et, al.

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著者別名 那須, 浩郎

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那須, 浩郎

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抄録
内容記述タイプ Abstract
内容記述 Along Hokkaido's Pacific coast near the town of Kiritappu, sandy deposits in a muddy lagoon and on a nearby beach-ridge plain provide evidence for 15 tsunamis between 200 and 6000 years ago. Additional sand beds at the lagoon probably represent the historical tsunamis of A.D. 1843 and 1894. We observed the sequences of sandy deposits in continuous slices 2 to 4 m deep. Some of the deposits consist of just a single sand bed, whereas others contain multiple units of sand, muddy sand (or sandy mud), and mud caps including plant detritus. We also found at the lagoon a 17th century tsunami deposit that thickens and thins regardless of elevation or distance inland. We bracketed the ages of most of the inferred tsunamis by radiocarbon dating of detritus, mainly seeds and leaves at the lagoon and charcoal at the beach-ridge plain, from pretsunami and posttsunami beds. Tsunami dates computed from the bracketing ages commonly have uncertainties spanning 2 to 4 centuries. Within these uncertainties, the inferred sequence of 15 prehistoric tsunamis at the lagoon, beginning almost 6000 years ago, can be matched tsunami by tsunami with the inferred history at the beach-ridge plain, 15 km away. The sand sheet extents suggest that most of these tsunamis were larger than any generated at Hokkaido in the last 200 years. The intervals between these inferred outsized tsunamis average nearly 400 years but range widely from about 100 to about 800 years.
書誌情報 Journal of Geophysical Research B: Solid Earth
en : Journal of Geophysical Research B: Solid Earth

巻 114, 号 1, p. B01319, 発行日 2009-01-04
出版者
出版者 Wiley-Blackwell
ISSN
収録物識別子タイプ ISSN
収録物識別子 01480227
DOI
識別子タイプ DOI
関連識別子 https://doi.org/10.1029/2007JB005503
関連名称 10.1029/2007JB005503
権利
権利情報 © 2009 by the American Geophysical Union
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