{"@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/1362544420807275776.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gca.2011.09.038"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S001670371100559X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S001670371100559X?httpAccept=text/plain"}}],"dc:title":[{"@value":"High-temperature Si isotope fractionation between iron metal and silicate"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544420807275780","@type":"Researcher","foaf:name":[{"@value":"Anat Shahar"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420807275648","@type":"Researcher","foaf:name":[{"@value":"Valerie J. Hillgren"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420807275777","@type":"Researcher","foaf:name":[{"@value":"Edward D. Young"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420807275779","@type":"Researcher","foaf:name":[{"@value":"Yingwei Fei"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420807275776","@type":"Researcher","foaf:name":[{"@value":"Catherine A. Macris"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420807275778","@type":"Researcher","foaf:name":[{"@value":"Liwei Deng"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-12","prism:volume":"75","prism:number":"23","prism:startingPage":"7688","prism:endingPage":"7697"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S001670371100559X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S001670371100559X?httpAccept=text/plain"}],"createdAt":"2011-10-03","modifiedAt":"2018-11-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232135623168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase relations in the system Fe–Ni–Si to 200 GPa and 3900 K and implications for Earth's core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390575661952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recent Progress in High‐Pressure Experiments on the Composition of the Core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710932894592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Perovskite in Earth’s deep interior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663334923136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isotopic signature of core-derived SiO2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663334934400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase transition boundary between fcc and hcp structures in Fe-Si alloy and its implications for terrestrial planetary cores"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266977826688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The chemical case for Mercury mantle stripping"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.gca.2011.09.038"},{"@type":"CROSSREF","@value":"10.1002/9781119526919.ch11_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"},{"@type":"CROSSREF","@value":"10.1126/science.aam8561_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"},{"@type":"CROSSREF","@value":"10.2138/am-2018-6482ccbyncnd_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"},{"@type":"CROSSREF","@value":"10.2138/am-2019-6636_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.01.056_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0312-z_references_DOI_RSsEjzeXsaRnS0Mq2DC5ITtdUM7"}]}