{"@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/1363388844971294976.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2013gl058678"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058678"}}],"dc:title":[{"@value":"Reexamination of the A.D. 869 Jogan earthquake size from tsunami deposit distribution, simulated flow depth, and velocity"}],"dcterms:alternative":[{"@value":"REEXAMINATION OF AD 869 JOGAN EARTHQUAKE"}],"description":[{"notation":[{"@value":"The rupture parameters and magnitude of the A.D. 869 Jogan earthquake, a predecessor of the 2011 Tohoku earthquake, were previously estimated by matching tsunami deposit distributions with simulated inundation areas. The tsunami inundation associated with the 2011 Tohoku earthquake, however, extended farther inland than the sandy tsunami deposits. Numerical simulation of the 2011 tsunami indicated that flow depths and velocities were approximately 1 m and 0.6 m/s, respectively, at the most inland sand deposit sites on the Ishinomaki and Sendai plains. While these values depend on the assumed bottom roughness, we used these values to compare tsunami deposits and inundation simulation of the 869 Jogan earthquake from both uniform-slip and 2011-type variable-slip fault models. The results showed that the rupture length of the 869 Jogan earthquake was at least 200 km and its minimum moment magnitude was 8.6."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844971294977","@type":"Researcher","foaf:name":[{"@value":"Yuichi Namegaya"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan; National Institute of Advanced Industrial Science and Technology; Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844971294976","@type":"Researcher","foaf:name":[{"@value":"Kenji Satake"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute; University of Tokyo; Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00948276"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2014-04-01","prism:volume":"41","prism:number":"7","prism:startingPage":"2297","prism:endingPage":"2303"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058678"}],"createdAt":"2014-01-16","modifiedAt":"2018-04-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813846346112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Examination of the largest-possible tsunamis (Level 2) generated along the Nankai and Suruga troughs during the past 4000years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"},{"@value":"Examination of the largest-possible tsunamis (Level 2 tsunami) generated along the Nankai and Suruga troughs during the past 4000 years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"}]},{"@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/1360002215916334976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Documenting large 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Japan"},{"@language":"ja-Kana","@value":"ミヤギケングマ ノ サク イセキ カラ ハッケン サレタ ジョウカン ジシン ニ ヨル ツナミ タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390288757502475520","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quantitative and semi–quantitative analyses using a portable energy dispersive X–ray fluorescence spectrometer: Geochemical applications in fault rocks, lake sediments, and event deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1390307114937721728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波堆積物に基づく波源推定の最近の展開"},{"@language":"en","@value":"Recent advances in deposit-based tsunami source modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238104256128","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Uncertainty in Tsunami Sediment Transport Modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1390571547634527744","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentological characteristics and distribution of tsunami deposits in shallow-marine sediments of Hirota Bay, Sanriku Rias, Japan"},{"@language":"ja","@value":"陸前高田市広田湾から確認された浅海域の津波堆積物の堆積学的特徴と分布"},{"@language":"ja-Kana","@value":"リクゼンタカタシ ヒロタワン カラ カクニン サレタ センカイイキ ノ ツナミ タイセキブツ ノ タイセキガクテキ トクチョウ ト ブンプ"}]},{"@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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