{"@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/1362825893569812352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.sedgeo.2012.05.004"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073812001418?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073812001418?httpAccept=text/plain"}}],"dc:title":[{"@value":"Relationship between the maximum extent of tsunami sand and the inundation limit of the 2011 Tohoku-oki tsunami on the Sendai Plain, Japan"}],"description":[{"notation":[{"@value":"Abstract   This paper focuses on the relationship between the maximum extent of sandy tsunami deposits and inundation distance of the 2011 Tohoku-oki tsunami. Inundation limits of the Tohoku-oki tsunami were assessed over seven shore-normal transects along the Sendai Coastal Plain. Inundation distances were found to range from 0.6 to 4.0 km. At the maximum extent of the tsunami deposit, the sand unit ranged in thicknesses from 0.1 to 4.0 cm. The maximum limit of the ≥ 0.5 cm thick sand layer extended to over 90% of the inundation distance where the inundation distance was less than 2.5 km. This observation is consistent with previous studies that examined characteristics of recent tsunami events that had inundation distances of at least 2 km. The maximum limit of the ≥ 0.5 cm thick sand layer extended to 3 km (57–76% of the inundation distance) where the inundation distance was more than 2.5 km. Our results are important for estimating paleo-tsunami inundation distances based on the landward extent of sand deposits and valuable for the assessment of future tsunami risks in other coastal areas in the world, which have been devastated by huge tsunamis in the past."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825893569812353","@type":"Researcher","foaf:name":[{"@value":"Tomoya Abe"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893569812354","@type":"Researcher","foaf:name":[{"@value":"Kazuhisa Goto"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893569812352","@type":"Researcher","foaf:name":[{"@value":"Daisuke Sugawara"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-12","prism:volume":"282","prism:startingPage":"142","prism:endingPage":"150"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0037073812001418?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0037073812001418?httpAccept=text/plain"}],"createdAt":"2012-05-23","modifiedAt":"2025-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335852005760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inverse Tsunami Flow Modeling Including Nonequilibrium Sediment Transport, With Application to Deposits From the 2011 Tohoku-Oki Tsunami"},{"@value":"Inverse Tsunami Flow Modeling Including Nonequilibrium Sediment Transport, With Application to Deposits From the 2011 Tohoku‐Oki Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001339198977664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological record of prehistoric tsunamis in Mugi town facing the Nankai Trough western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050011495267202560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstruction of flow conditions from 2004 Indian Ocean tsunami deposits at the Phra Thong island using a deep neural network inverse model"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810730081920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentary features observed in the tsunami deposits at Rikuzentakata 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