{"@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/1363670320247473920.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0040-1951(87)90333-7"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195187903337?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195187903337?httpAccept=text/plain"}}],"dc:title":[{"@value":"Flow properties of continental lithosphere"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320247473921","@type":"Researcher","foaf:name":[{"@value":"Neville L. Carter"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320247473920","@type":"Researcher","foaf:name":[{"@value":"Michael C. Tsenn"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1987-05","prism:volume":"136","prism:number":"1-2","prism:startingPage":"27","prism:endingPage":"63"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0040195187903337?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0040195187903337?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001206514107648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Postseismic deformation and the strength of ductile shear zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488768000","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Acceleration of slip motion in deep extensions of seismogenic faults in and below the seismogenic region"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564237990897152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻変動からマグマ溜まりを推論する"},{"@language":"en","@value":"Crustal Deformation Infers a Magma Chamber"},{"@language":"ja-Kana","@value":"チカク ヘンドウ カラ マグマ タマリ オ スイロン スル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390870529360676096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北沖地震の余効変動から知る東北日本弧地殻マントルのレオロジー特性"},{"@language":"en","@value":"Rheological Properties of the Crust and Upper Mantle in Northeast Japan Following Postseismic Deformation from the 2011 Tohoku-oki Earthquake"},{"@value":"東北沖地震の余効変動から知る東北日本孤地殻マントルのレオロジー特性"},{"@language":"ja-Kana","@value":"トウホクオキ ジシン ノ ヨコウヘンドウ カラ シル トウホク ニホンコチカク マントル ノ レオロジー トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066368640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0040-1951(87)90333-7"},{"@type":"CROSSREF","@value":"10.1186/bf03353332_references_DOI_8bE66ZhyEsa6HhmRuDLGIn8reC6"},{"@type":"CROSSREF","@value":"10.5026/jgeography.135.61_references_DOI_8bE66ZhyEsa6HhmRuDLGIn8reC6"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00539-1_references_DOI_8bE66ZhyEsa6HhmRuDLGIn8reC6"},{"@type":"CROSSREF","@value":"10.1186/bf03353320_references_DOI_8bE66ZhyEsa6HhmRuDLGIn8reC6"},{"@type":"CROSSREF","@value":"10.5026/jgeography.127.111_references_DOI_8bE66ZhyEsa6HhmRuDLGIn8reC6"}]}