{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361981471284302848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03352848"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03352848.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03352848/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03352848"}}],"dc:title":[{"@value":"Fault models of unusual tsunami in the 17th century along the Kuril trench"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Geologic evidence has shown that unusual tsunami deposits are traced as high as 18 m above the current sea level or as far as 1–4 km inland from the shoreline on the Pacific coast of eastern Hokkaido, and that such unusual tsunamis have recurred at about 500 year interval with the most recent event in the 17th century. We computed coastal tsunami heights along the Hokkaido and Sanriku coasts and inundation at five coastal marshes in Hokkaido where the tsunami deposits were mapped. Three types of faults were tested: giant fault, tsunami earthquake and interplate earthquake models. The giant fault model, with the largest seismic moment, yields the lowest tsunami heights and smaller inundation than the distribution of tsunami deposits in Hokkaido, while the tsunami heights are largest in Sanriku. The tsunami earthquake model yields little inundation in Hokkaido and the smallest heights in Sanriku. The interplate earthquake model produces the largest tsunami heights and inundation in Hokkaido, reproducing the distribution of tsunami deposits on the Nemuro coast. The multi-segment interplate earthquake with variable slip (10 m on Tokachi and 5 m on Nemuro segment) can reproduce the distribution of tsunami deposits on the Tokachi coast as well, and considered as the best source model for the 17th century tsunami, although the Sanriku tsunami heights are more than 3 m, exceeding an inferred detection threshold of historical documents. The seismic moment is estimated as 8 × 10<jats:sup>21</jats:sup>N m (<jats:italic>M</jats:italic><jats:sub>w</jats:sub>8.5). Comparison with the recent 2003 Tokachi-oki earthquake indicates that the 17th century tsunami source was longer and located further offshore at shallower depth.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017280649935381","@type":"Researcher","foaf:name":[{"@value":"K. Satake"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471284302848","@type":"Researcher","foaf:name":[{"@value":"F. Nanayama"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471284302849","@type":"Researcher","foaf:name":[{"@value":"S. Yamaki"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2008-09","prism:volume":"60","prism:number":"9","prism:startingPage":"925","prism:endingPage":"935"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0/","https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/BF03352848.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03352848/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03352848"}],"createdAt":"2014-08-15","modifiedAt":"2022-04-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564285794447232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of postseismic deformation following the 2003 Tokachi-oki earthquake and estimation of the viscoelastic structure in Hokkaido, northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050585658871539712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"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"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587041605699968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Authentic fault models and dispersive tsunami simulations for outer-rise normal earthquakes in the southern Kuril Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456405726464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Method for Near-Real Time Estimation of Tsunami Sources Using Ocean Bottom Pressure Sensor Network (S-Net)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709607680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Challenges of anticipating the 2011 Tohoku earthquake and tsunami using coastal geology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324606464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2011 Tohoku earthquake (Mw 9.0) sequence and subduction dynamics in Western Pacific and East Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232352897792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sediment transport modeling of multiple grain sizes for the 2011 Tohoku tsunami on a steep coastal valley of Numanohama, northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516799846528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dating tsunami deposits: Present knowledge and challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005521267397760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evidence of giant earthquakes and tsunamis of the seventeenth-century type along the southern Kuril subduction zone, eastern Hokkaido, northern Japan: a review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168825818368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleotsunami history along the northern Japan trench based on sequential dating of the continuous geological record potentially inundated only by large tsunamis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870541779968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial Extent of Mid‐To Late‐Holocene Sedimentary Record of Tsunamis Along the Southern Kuril Trench, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280649935360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Scour ponds from unusually large tsunamis on a beach-ridge plain in eastern Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283692753624448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological and historical evidence of irregular recurrent earthquakes in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360303782143371136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"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"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869739008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Re-estimated fault model of the 17th century great earthquake off Hokkaido using tsunami deposit data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166090663680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of topography on particle composition of 2011 tsunami deposits on the ria-type Sanriku coast, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183245672576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interplate Slip Following the 2003 Tokachi‐oki Earthquake From Ocean Bottom Pressure Gauge and Land GNSS Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092458494080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical modeling of tsunami: advances and future challenges after the 2011 Tohoku earthquake and tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230599303424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological record of 18th and 19th century tsunamis along the Japan Sea coast of Tsugaru Peninsula, northwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861294960275072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sediment Transport Modeling Based on Geological Data for Holocene Coastal Evolution: Wave Source Estimation of Sandy Layers on the Coast of Hidaka, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815502303360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New source model for the 1771 Meiwa tsunami along the southern Ryukyu Trench inferred from high-resolution tsunami calculation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240893568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review of previous studies on tsunami deposits in Hokkaido, northern Japan:Focusing on the studies of deposits from 17th century large tsunamis and others"},{"@language":"ja","@value":"北海道の津波堆積物研究の現状と課題：17世紀巨大津波による堆積物の研究を中心に"},{"@language":"ja-Kana","@value":"ホッカイドウ ノ ツナミ タイセキブツ ケンキュウ ノ ゲンジョウ ト カダイ : 17セイキ キョダイ ツナミ ニ ヨル タイセキブツ ノ ケンキュウ オ チュウシン ニ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216836224","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleotsunami research along the Pacific coast of Tohoku region"},{"@language":"ja","@value":"東北地方太平洋側における古津波堆積物の研究"},{"@language":"ja-Kana","@value":"トウホク チホウ タイヘイヨウガワ ニ オケル コ ツナミ タイセキブツ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216916992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review of the studies of tsunami deposit of Hokkaido, northern Japan:"},{"@language":"ja","@value":"北海道太平洋岸の津波堆積物研究："},{"@value":"北海道太平洋岸の津波堆積物研究 : 北方四島の津波堆積物と北海道西部太平洋側の断層モデルの検討"},{"@language":"ja-Kana","@value":"ホッカイドウ タイヘイヨウガン ノ ツナミ タイセキブツ ケンキュウ : ホッポウ ヨントウ ノ ツナミ タイセキブツ ト ホッカイドウ セイブ タイヘイヨウガワ ノ ダンソウ モデル ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218549120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Study on paleotsunami deposits in geologic stratum"},{"@language":"ja","@value":"地層中に存在する古津波堆積物の調査"},{"@language":"ja-Kana","@value":"チソウ チュウ ニ ソンザイ スル コ ツナミ タイセキブツ ノ チョウサ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681471816064","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Event deposits on the Pacific coast of Misawa, Aomori Prefecture, northern Japan"},{"@language":"ja","@value":"青森県三沢市で検出されたイベント堆積物"},{"@language":"ja-Kana","@value":"アオモリケン ミサワシ デ ケンシュツ サレタ イベント タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472966656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"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"},{"@language":"en","@value":"Identification of a 17th-century tsunami deposit on the northern Hidaka coast, Hokkaido, northern Japan"},{"@language":"ja-Kana","@value":"ホッカイドウ ヒダカ カイガン ホクブ カラ カクニン サレタ 17セイキ ノ ツナミ タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390288547260720768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"大規模波動イベントの影響を繰り返し受けたカキ礁の破壊と復元過程：北海道東部，馬主来沼における完新統<i>Crassostrea gigas </i>化石密集層の例"},{"@language":"en","@value":"Destruction and restoration processes of fossil oyster reef influenced by repeated large-scale waves: An example of Holocene Crassostrea gigas shellbeds around Pashukurutou Lagoon, eastern Hokkaido, northeast Japan"},{"@value":"大規模波動イベントの影響を繰り返し受けたカキ礁の破壊と復元過程 : 北海道東部,馬主来沼における完新統Crassostrea gigas化石密集層の例"},{"@language":"ja-Kana","@value":"ダイキボ ハドウ イベント ノ エイキョウ オ クリカエシ ウケタ カキショウ ノ ハカイ ト フクゲン カテイ : ホッカイドウ トウブ,バシュライヌマ ニ オケル カンシントウCrassostrea gigas カセキ ミッシュウソウ ノ レイ"},{"@value":"Destruction and restoration processes of fossil oyster reef influence by repeated large-scale waves: an example of Holocene Crassostrea gigas shellbeds around Pashukurutou Lagoon, eastern Hokkaido, northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390296906985889408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimating the Sources for 17th Century Tsunami by Using Tsunami Deposits Distributed from the Northern Hidaka Coast to Uchiura Bay, Hokkaido, Japan"},{"@language":"ja","@value":"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"},{"@language":"ja-Kana","@value":"ホッカイドウ ヒダカ カイガン ホクブ カラ ウチウラワン シュウヘン ニ ブンプ スル 17セイキ ノ ツナミ タイセキブツ オ サイゲン スル ツナミハ ゲン ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238103264768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Real-Time Tsunami Inundation Forecast for a Recurrence of 17<sup>th</sup> Century Great Hokkaido Earthquake in Japan"},{"@value":"Real-Time Tsunami Inundation Forecast for a Recurrence of 17th Century Great Hokkaido Earthquake in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713073824896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On tsunami sediment transport modeling and uncertainties"},{"@language":"ja","@value":"津波土砂移動数値解析の不確実性と地形復元について"},{"@language":"ja-Kana","@value":"ツナミ ドシャ イドウ スウチ カイセキ ノ フカクジツセイ ト チケイ フクゲン ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713079952000","@type":"Article","resourceType":"学術雑誌論文(journal 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