Numerical estimation of a tsunami source at the flexural area of Kuril and Japan Trenches in the fifteenth to seventeenth century based on paleotsunami deposit distributions in northern Japan
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-022-00530-2]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- Kai SatoMasaki YamadaDaisuke Ishimura
- 出版年月日等
- 2022-12-22
- 出版年（W3CDTF）
- 2022-12-22
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(72)
- 掲載巻
- 9(72)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00530-2
- 国立国会図書館永続的識別子
- info:ndljp/pid/12998713
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2023-09-27T14:40:47+09:00
- 保存日（W3CDTF）
- 2023-04-11
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/12307811
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- Paleotsunami deposit investigations and numerical tsunami computations have been performed to elucidate the source and size of large tsunamis along the Kuril to Japan Trenches, particularly for unusual tsunamis that occurred in the seventeenth century, the 1611 CE Keicho tsunami (M 8.1) along the Japan Trench and seventeenth-century tsunami (> Mw 8.8) along the Kuril Trench, which caused serious damages on the coastal residents and environments. Moreover, several paleotsunami deposits dating from the thirteenth to eighteenth centuries have been reported along the area between the Kuril and Japan subduction zones, but their sources have not been clarified. In this study, we estimated the tsunami sources from numerical simulations using the distribution of fifteenth- to seventeenth-century tsunami deposits at Sekinehama along the coast of the Shimokita Peninsula. Based on numerical simulations with previously proposed fault models, the tsunami deposits showing similar ages at Sekinehama and another site on the coast of Shimokita Peninsula, which are within 50 km apart, could not be explained except with the huge earthquake models (> Mw 9.1), whose rupture zones extend to not only the Kuril or Japan Trenches but also their flexural area. Thus, we modified or newly proposed twelve fault models located in the flexural area between the two trenches to explain tsunami deposits possibly around the seventeenth century at the above-mentioned two sites on the coast of Shimokita Peninsula. Simulations using these models elucidated that the rupture in the shallow or deep plate boundaries with > 14–32 m slip (> Mw 8.55–8.76) is necessary. If the tsunami deposits around the seventeenth century along the Iburi–Hidaka coast in Hokkaido and those at the two sites mentioned above might be left by an identical event, an interplate earthquake with > 18–40 m slip (> Mw 8.62–9.2) in the flexural area is needed. Moreover, this interplate earthquake might have occurred in the deep plate boundary than in the shallower plate boundary based on slip deficit and slow earthquake distribution data. Our results offer significant insights into a large earthquake (> M 8) along the Kuril and Japan Trenches in the fifteenth to seventeenth century.
- DOI
- 10.1186/s40645-022-00530-2
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
- 関連情報（URI）
- 参照
- High-precision estimation of a paleo-tsunami inundation area by identifying tsunami traces beyond sandy tsunami deposits: A case study of the 869 CE Jogan tsunami in Fukushima, northeastern Japan北海道日高海岸北部から内浦湾周辺に分布する17世紀の津波堆積物を再現する津波波源の推定
- 参照
- Inverse Tsunami Flow Modeling Including Nonequilibrium Sediment Transport, With Application to Deposits From the 2011 Tohoku‐Oki TsunamiConnecting slow earthquakes to large earthquakesParallel Implementation of Dispersive Tsunami Wave Modeling with a Nesting Algorithm for the 2011 Tohoku TsunamiChallenges of anticipating the 2011 Tohoku earthquake and tsunami using coastal geologyRe-examination of the age of historical and paleo-tsunami deposits at Koyadori on the Sanriku Coast, Northeast JapanIdentification and possible recurrence of an oversized tsunami on the Pacific coast of northern JapanThe slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatoriesUnusually large earthquakes inferred from tsunami deposits along the Kuril trenchGlobal topography and bathymetry grid improves research effortsPaleotsunami history along the northern Japan trench based on sequential dating of the continuous geological record potentially inundated only by large tsunamisHistorical tsunami and storm deposits during the last five centuries on the Sanriku coast, JapanCoseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic dataNationwide Post Event Survey and Analysis of the 2011 Tohoku Earthquake TsunamiSpatial distribution of the faulting types of small earthquakes around the 2011 Tohoku‐oki earthquake: A comprehensive search using template eventsTsunami history over the past 2000 years on the Sanriku coast, Japan, determined using gravel deposits to estimate tsunami inundation behaviorEstimation of Tsunami Characteristics from Deposits: Inverse Modeling Using a Deep‐Learning Neural NetworkShorter intervals between great earthquakes near Sendai: Scour ponds and a sand layer attributable to <scp>A.D.</scp> 1454 overwashHistorical and geological evidence for the seventeenth-century tsunamis along Kuril and Japan trenches: implications for the origin of the AD 1611 Keicho earthquake and tsunami, and for the probable future risk potentialGeological evidence for an unusually large tsunami on the Pacific coast of Aomori, northern JapanTraces of Tsunami Preserved in Inter-Tidal Lacustrine and Marsh Deposits: Some Examples from Northeast JapanSurface deformation due to shear and tensile faults in a half-spaceRe-estimated fault model of the 17th century great earthquake off Hokkaido using tsunami deposit dataHolocene environmental changes and paleo-tsunami history in Onuma on the southern part of the Sanriku Coast, northeast JapanNumerical modeling of tsunami: advances and future challenges after the 2011 Tohoku earthquake and tsunamiTen years after the 2011 Tohoku-oki earthquake and tsunami: Geological and environmental effects and implications for disaster policy changesAperiodic recurrence of geologically recorded tsunamis during the past 5500 years in eastern Hokkaido, JapanNine unusually large tsunami deposits from the past 4000 years at Kiritappu marsh along the southern Kuril TrenchAssessing the magnitude of the 869 Jogan tsunami using sedimentary deposits: Prediction and consequence of the 2011 Tohoku-oki tsunamiThe Generic Mapping Tools Version 6Transient Uplift After a 17th-Century Earthquake Along the Kuril Subduction ZoneStratigraphy, distribution, and petrographic properties of Holocene tephras in Hokkaido, northern JapanFault models of unusual tsunami in the 17th century along the Kuril trenchInterplate coupling beneath NE Japan inferred from three‐dimensional displacement fieldTsunami generation by horizontal displacement of ocean bottomLiquefaction as an important source of the A.D. 2011 Tohoku-oki tsunami deposits at Sendai Plain, JapanReexamination of the A.D. 869 Jogan earthquake size from tsunami deposit distribution, simulated flow depth, and velocityTsunami deposits from the 1993 Southwest Hokkaido earthquake and the 1640 Hokkaido Komagatake eruption, northern JapanNew insights of tsunami hazard from the 2011 Tohoku-oki eventOn the Need for Larger Manning's Roughness Coefficients in Depth-Integrated Tsunami Inundation Models下北半島北西端周辺の地震性隆起海岸地形と 海底活断層Tsunami run-up heights of the 2003 Tokachi-oki earthquake三陸沖における再来大地震の震源過程の比較研究仙台平野における貞観11年 (869年) 三陸津波の痕跡高の推定北海道胆振海岸東部から確認された１７世紀の津波堆積物北海道日高海岸北部から確認された17世紀の津波堆積物Reliability of tsunami source model derived from fault parameters北海道津軽海峡沿岸域で認められたイベント堆積物1640年北海道駒ヶ岳噴火による津波堆積物の分布と津波規模の推定Global tsunami Terrain ModelWashover deposits related to tsunami and storm surge along the north coast of the Shimokita Peninsula in northern JapanShort-wave run-ups of the 1611 Keicho tsunami along the Sanriku CoastSpatial distribution and sources of tsunami deposits in a narrow valley setting - insight from 2011 Tohoku-oki tsunami deposits in northeastern JapanHistorical and paleo-tsunami deposits during the last 4000 years and their correlations with historical tsunami events in Koyadori on the Sanriku Coast, northeastern Japan
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossref
- 書誌ID（NDLBibID）
- 12998713