{"@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/1361699994972794752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2012.06.006"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195112003125?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195112003125?httpAccept=text/plain"}}],"dc:title":[{"@value":"Faults (shear zones) in the Earth's mantle"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994972794753","@type":"Researcher","foaf:name":[{"@value":"Alain Vauchez"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994972794752","@type":"Researcher","foaf:name":[{"@value":"Andréa Tommasi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994972794754","@type":"Researcher","foaf:name":[{"@value":"David Mainprice"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-08","prism:volume":"558-559","prism:startingPage":"1","prism:endingPage":"27"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195112003125?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195112003125?httpAccept=text/plain"}],"createdAt":"2012-06-15","modifiedAt":"2019-06-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1361131417223027072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Creep mechanisms in the lithospheric mantle inferred from deformation of iron-free forsterite aggregates at 900–1200 °C"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.tecto.2012.06.006"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2019.04.009_references_DOI_CPU28EacwGWNb2CATkdHjLuF8hm"}]}