{"@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/1363388843566798464.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2010.01.004"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X10000233?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X10000233?httpAccept=text/plain"}}],"dc:title":[{"@value":"Sr–Nd–Os evidence for a stable erosion regime in the Himalaya during the past 12Myr"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388843566798467","@type":"Researcher","foaf:name":[{"@value":"Valier Galy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843566798464","@type":"Researcher","foaf:name":[{"@value":"Christian France-Lanord"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843566798465","@type":"Researcher","foaf:name":[{"@value":"Bernhard Peucker-Ehrenbrink"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843566798466","@type":"Researcher","foaf:name":[{"@value":"Pascale Huyghe"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2010-02","prism:volume":"290","prism:number":"3-4","prism:startingPage":"474","prism:endingPage":"480"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X10000233?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X10000233?httpAccept=text/plain"}],"createdAt":"2010-01-26","modifiedAt":"2018-12-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360290617877406976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Miocene provenance change in Himalayan foreland basin and Bengal Fan sediments, with special reference to detrital garnet chemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379378512512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Miocene Uplift and Exhumation of the Lesser Himalaya Recorded by Clumped Isotope Compositions of Detrital Carbonate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656146981248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Determining sources of deep-sea mud by organic matter signatures in the Sunda trench and Aceh basin off Sumatra"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367089648512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomorphological processes and their connectivity in hillslope, fuvial, and coastal areas in Bangladesh : a review"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.epsl.2010.01.004"},{"@type":"CROSSREF","@value":"10.1111/iar.12408_references_DOI_VS33BjREXzeeimCECiiUyG1gQGC"},{"@type":"CROSSREF","@value":"10.1029/2024gl109643_references_DOI_VS33BjREXzeeimCECiiUyG1gQGC"},{"@type":"CROSSREF","@value":"10.1007/s00367-017-0510-x_references_DOI_VS33BjREXzeeimCECiiUyG1gQGC"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00500-8_references_DOI_VS33BjREXzeeimCECiiUyG1gQGC"}]}