{"@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/1361981470567300352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s00531-014-1032-7"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00531-014-1032-7.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s00531-014-1032-7/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00531-014-1032-7"}}],"dc:title":[{"@value":"Detrital zircon U–Pb ages of Late Triassic–Late Jurassic deposits in the western and northern Sichuan Basin margin: constraints on the foreland basin provenance and tectonic implications"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981470567300226","@type":"Researcher","foaf:name":[{"@value":"Liang Luo"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470567300353","@type":"Researcher","foaf:name":[{"@value":"Jia-Fu Qi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470567300225","@type":"Researcher","foaf:name":[{"@value":"Ming-Zheng Zhang"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470567300224","@type":"Researcher","foaf:name":[{"@value":"Kai Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470567300352","@type":"Researcher","foaf:name":[{"@value":"Yu-Zhen Han"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"14373254"},{"@type":"EISSN","@value":"14373262"}],"prism:publicationName":[{"@value":"International Journal of Earth Sciences"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2014-05-20","prism:volume":"103","prism:number":"6","prism:startingPage":"1553","prism:endingPage":"1568"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s00531-014-1032-7.pdf"},{"@id":"http://link.springer.com/article/10.1007/s00531-014-1032-7/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s00531-014-1032-7"}],"createdAt":"2014-05-19","modifiedAt":"2019-05-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2050588891962967808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signal intensity of quartz in the fine-silt fraction of riverbed sediments from the Yangtze River : a provenance tracer for suspended particulate matter"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s00531-014-1032-7"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0118-9_references_DOI_TYe6lV8dCYbQ84yoelW3sQeQr0q"}]}