{"@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/1363670320070522880.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.quascirev.2011.03.015"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0277379111000874?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0277379111000874?httpAccept=text/plain"}}],"dc:title":[{"@value":"Tephrochronology of the Siple Dome ice core, West Antarctica: correlations and sources"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320070522881","@type":"Researcher","foaf:name":[{"@value":"Nelia W. Dunbar"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320070522880","@type":"Researcher","foaf:name":[{"@value":"Andrei V. Kurbatov"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02773791"}],"prism:publicationName":[{"@value":"Quaternary Science Reviews"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-06","prism:volume":"30","prism:number":"13-14","prism:startingPage":"1602","prism:endingPage":"1614"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0277379111000874?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0277379111000874?httpAccept=text/plain"}],"createdAt":"2011-05-08","modifiedAt":"2020-05-06","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360857593652763392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Antarctic surface temperature and elevation during the Last Glacial Maximum"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418768277760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367122683264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volcanic ash in bare ice south of Sør Rondane Mountains, Antarctica : geochemistry, rock magnetism and nondestructive magnetic detection with SQUID gradiometer"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2011.03.015"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0415-3_references_DOI_DgNEVEmIHEhiQnfkl8uEwDOMMf8"},{"@type":"CROSSREF","@value":"10.1126/science.abd2897_references_DOI_DgNEVEmIHEhiQnfkl8uEwDOMMf8"},{"@type":"CROSSREF","@value":"10.1073/pnas.1902469117_references_DOI_DgNEVEmIHEhiQnfkl8uEwDOMMf8"}]}