{"@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/1362825893606663168.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s00024-006-0164-5"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00024-006-0164-5.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s00024-006-0164-5/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00024-006-0164-5"}}],"dc:title":[{"@value":"The 26 December 2004 Sumatra Tsunami: Analysis of Tide Gauge Data from the World Ocean Part 1. Indian Ocean and South Africa"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825893606663169","@type":"Researcher","foaf:name":[{"@value":"Alexander B. Rabinovich"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893606663168","@type":"Researcher","foaf:name":[{"@value":"Richard E. Thomson"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00334553"},{"@type":"EISSN","@value":"14209136"}],"prism:publicationName":[{"@value":"Pure and Applied Geophysics"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2007-01-30","prism:volume":"164","prism:number":"2-3","prism:startingPage":"261","prism:endingPage":"308"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s00024-006-0164-5.pdf"},{"@id":"http://link.springer.com/article/10.1007/s00024-006-0164-5/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s00024-006-0164-5"}],"createdAt":"2007-02-02","modifiedAt":"2019-05-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050587981429018368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215254647552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New Insights into the Source of the Makran Tsunami of 27 November 1945 from Tsunami Waveforms and Coastal Deformation Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231143680896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Time–Frequency Characteristics of Tsunami Magnetic Signals from Four Pacific Ocean Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291076608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami Waves and Tsunami‐Induced Natural Oscillations Determined by HF Radar in Ise Bay, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282240600448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of Tsunami Data to the Up-Dip Extent of the July 2021 Mw 8.2 Alaska Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706120339968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep-Water Characteristics of the Trans-Pacific Tsunami from the 1 April 2014 M w 8.2 Iquique, Chile Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270427550464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"History and features of trans-oceanic tsunamis and implications for paleo-tsunami studies"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s00024-006-0164-5"},{"@type":"CROSSREF","@value":"10.1007/s00024-014-0948-y_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1007/s00024-016-1345-5_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1029/2017jc013626_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1785/0220210359_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1007/s00024-014-0983-8_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0278-x_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2020.103112_references_DOI_UK4T7akEXCwIVhGmonwk06y0Lhv"}]}