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  1. B. 理工学域; 数物科学類・物質化学類・機械工学類・フロンティア工学類・電子情報通信学類・地球社会基盤学類・生命理工学類
  2. b 10. 学術雑誌掲載論文
  3. 1.査読済論文(理)

Fossil tubeworms link coastal uplift of the northern Noto Peninsula to rupture of the Wajima-oki fault in AD 1729

https://doi.org/10.24517/00010783
https://doi.org/10.24517/00010783
5af2ac26-60ab-4349-9eec-6b345f3d9a92
名前 / ファイル ライセンス アクション
SC-PR-HAMADA-M-38.pdf SC-PR-HAMADA-M-38.pdf (956.1 kB)
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Item type 学術雑誌論文 / Journal Article(1)
公開日 2017-12-05
タイトル
タイトル Fossil tubeworms link coastal uplift of the northern Noto Peninsula to rupture of the Wajima-oki fault in AD 1729
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
ID登録
ID登録 10.24517/00010783
ID登録タイプ JaLC
著者 Hamada, Masaaki

× Hamada, Masaaki

WEKO 68808

Hamada, Masaaki

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Hiramatsu, Yoshihiro

× Hiramatsu, Yoshihiro

WEKO 198
e-Rad 80283092
金沢大学研究者情報 80283092
研究者番号 80283092

Hiramatsu, Yoshihiro

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Oda, Mitsuhiro

× Oda, Mitsuhiro

WEKO 68809

Oda, Mitsuhiro

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Yamaguchi, Hiroyuki

× Yamaguchi, Hiroyuki

WEKO 68810

Yamaguchi, Hiroyuki

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著者別表示 平松, 良浩

× 平松, 良浩

平松, 良浩

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書誌情報 Tectonophysics

巻 670, p. 38-47, 発行日 2016-02-22
ISSN
収録物識別子タイプ ISSN
収録物識別子 0040-1951
NCID
収録物識別子タイプ NCID
収録物識別子 AA00860886
出版者
出版者 Elsevier
抄録
内容記述タイプ Abstract
内容記述 The active fault zone on the seafloor off the northern coast of the Noto Peninsula of central Japan is divided into four segments from west to east: Monzen-oki, Saruyama-oki, Wajima-oki, and Suzu-oki. To examine the latest event that occurred in these segments, we investigated the dates and elevations of fossilized intertidal tubeworms along the northern coast of the Noto Peninsula, located on the hanging-wall sides of the faults, using radioactive carbon dating and global positioning measurements. For each fossil, we calculated the difference between the past and present elevation, thereby estimating the elevation of the sea level at the date of the fossil, using a curve for sea level change. This calculation provided us with the elevation change at each site. The vertical changes estimated from the elevations and ages of the intertidal tubeworms revealed that the coastal emergence probably occurred between 1600 and 1800 AD. This area of coastal emergence lies adjacent to active faults within the Wajima-oki segment. A model for rectangular faults with three fault planes and a moment magnitude of 6.6 for the Wajima-oki segment reproduced the observed pattern of coastal emergence well. Only one damaging earthquake, that in 1729, is known to have occurred in this part of the northern Noto Peninsula between 1600 and 1800 AD, and there has not been one since 1800 AD. The slip distribution of the fault predicted by the model is consistent with the distribution of shaking-related damage documented in 1729. We conclude that rupture of the Wajima-oki segment caused the 1729 earthquake. © 2016 Elsevier B.V.
内容記述
内容記述タイプ Other
内容記述 Embargo Period 24 months
権利
権利情報 Copyright © Elsevier (CC-BY NC ND)
著者版フラグ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
関連URI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 10.1016/j.tecto.2015.12.019
関連URI
関連タイプ isIdenticalTo
識別子タイプ URI
関連識別子 http://www.elsevier.com/locate/issn/00401951
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