{"@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/1362825896086076416.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gca.2012.01.010"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703712000336?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703712000336?httpAccept=text/plain"}}],"dc:title":[{"@value":"Metal–silicate partitioning of Mo and W at high pressures and temperatures: Evidence for late accretion of sulphur to the Earth"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896086076417","@type":"Researcher","foaf:name":[{"@value":"Jon Wade"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896086076416","@type":"Researcher","foaf:name":[{"@value":"Bernard J. Wood"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896086076418","@type":"Researcher","foaf:name":[{"@value":"James Tuff"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-05","prism:volume":"85","prism:startingPage":"58","prism:endingPage":"74"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0016703712000336?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0016703712000336?httpAccept=text/plain"}],"createdAt":"2012-01-30","modifiedAt":"2018-11-26","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567179761000448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High Pressure Experiments on Metal‐Silicate Partitioning of Chlorine in a Magma Ocean: Implications for Terrestrial Chlorine Depletion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092855479552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermodynamical Modeling of Liquid Fe‐Si‐Mg‐O:Molten Magnesium Silicate Release From the Core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576217166865536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Light elements in the Earth’s core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656128772352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase relations in the carbon-saturated C–Mg–Fe–Si–O system and C and Si solubility in liquid Fe at high pressure and temperature: implications for planetary interiors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567489302912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earth and Mars – Distinct inner solar system products"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975841797209344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multi-element isotope study of natrocarbonatites (1993 lava flows) from Oldoinyo Lengai volcano, Tanzania: Implications for core-mantle interactions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681521485184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The reactions between iron and magnesite at 6 GPa and 1273–1873 K: Implication to reduction of subducted carbonate in the deep mantle"}]},{"@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.2012.01.010"},{"@type":"CROSSREF","@value":"10.1038/s43017-021-00203-6_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1016/j.jafrearsci.2019.103725_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1002/2017gc007159_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.2465/jmps.141003a_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1029/2020gl089218_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1007/s00269-013-0600-x_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1016/j.chemer.2021.125746_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0312-z_references_DOI_4Ozo7zSpvTZQHkYz5bbCcEKUNUO"}]}