{"@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/1361699996409387392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.palaeo.2006.11.024"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018206006961?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018206006961?httpAccept=text/plain"}}],"dc:title":[{"@value":"Age of the SKP-I and SKP-II tephras from the southern East Sea/Japan Sea: Implications for interstadial events recorded in sediment from marine isotope stages 3 and 4"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699996409387395","@type":"Researcher","foaf:name":[{"@value":"Jong-Hwa Chun"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699996409387394","@type":"Researcher","foaf:name":[{"@value":"Daekyo Cheong"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699996409387392","@type":"Researcher","foaf:name":[{"@value":"Ken Ikehara"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699996409387393","@type":"Researcher","foaf:name":[{"@value":"Sang-Joon Han"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2007-04","prism:volume":"247","prism:number":"1-2","prism:startingPage":"100","prism:endingPage":"114"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031018206006961?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031018206006961?httpAccept=text/plain"}],"createdAt":"2007-01-09","modifiedAt":"2019-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360283691114260096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Integrating the Holocene tephrostratigraphy for East Asia using a high-resolution cryptotephra study from Lake Suigetsu (SG14 core), central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691180784512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Quaternary tephrostratigraphy of Baegdusan and Ulleung Volcanoes using marine sediments in the Japan Sea/East Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380131147776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A detailed record of large explosive eruptions from Japan between ∼120 and 50 ka preserved at Lake Suigetsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891977264640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East Asia) over the last 86 kyrs using distal sedimentary records"}]},{"@id":"https://cir.nii.ac.jp/crid/1390013043977303424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pleistocene to Holocene tephrastratigraphy in the off Wakasa Bay sediment cores and correlation with widespread tephras"},{"@language":"ja","@value":"若狭湾沖海底堆積物コアに挟まる後期更新世から完新世テフラの層序と広域テフラとの対比"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842097198848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine tephra in the Japan Sea sediments as a tool for paleoceanography and paleoclimatology"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2006.11.024"},{"@type":"CROSSREF","@value":"10.1016/j.yqres.2013.04.002_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0068-z_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2024.109021_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2019.106669_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"},{"@type":"CROSSREF","@value":"10.4116/jaqua.61.2111_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2017.12.013_references_DOI_JUtfR3MNohcRCJiX6x8EtVcxIMF"}]}