{"@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/1361699995791848192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jsg.2008.01.008"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814108000175?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814108000175?httpAccept=text/plain"}}],"dc:title":[{"@value":"Relationships between faults, extension fractures and veins, and stress"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711829031686","@type":"Researcher","foaf:name":[{"@value":"T.G. Blenkinsop"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2008-05","prism:volume":"30","prism:number":"5","prism:startingPage":"622","prism:endingPage":"632"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0191814108000175?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0191814108000175?httpAccept=text/plain"}],"createdAt":"2008-01-28","modifiedAt":"2019-01-01","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360283690913952640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Exploring the structural controls on helium, nitrogen and carbon isotope signatures in hydrothermal fluids along an intra-arc fault system"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942188138368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multiple damage zone structure of an exhumed seismogenic megasplay fault in a subduction zone : a study from the Nobeoka Thrust Drilling Project"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892145535616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Laboratory evidence of strength recovery of a healed fault : implications for a mechanism responsible for creating wide fault zones"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.jsg.2008.01.008"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0377-x_references_DOI_EtoiAbBK5CeDOP9mQ9uk9wOPCC"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0186-2_references_DOI_EtoiAbBK5CeDOP9mQ9uk9wOPCC"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2016.04.031_references_DOI_EtoiAbBK5CeDOP9mQ9uk9wOPCC"}]}