{"@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/1363388843597540224.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1233514"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1233514"}}],"dc:title":[{"@value":"Melting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray Diffraction"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Hot Enough to Melt Iron</jats:title>\n          <jats:p>\n            Earth's core is divided into a fluid outer core and a solid inner core, both composed predominately of iron at extremely high pressures and temperatures. The boundary between these two regions is largely controlled by the melting point of iron at ∼330 GPa, which in turn influences heat transfer and geodynamo generation.\n            <jats:bold>\n              Anzellini\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6131\" page=\"464\" related-article-type=\"in-this-issue\" vol=\"340\" xlink:href=\"10.1126/science.1233514\">464</jats:related-article>\n            , see the Perspective by\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6131\" page=\"442\" related-article-type=\"in-this-issue\" vol=\"340\" xlink:href=\"10.1126/science.1236304\">Fei</jats:related-article>\n            ) compressed iron in a laser-heated diamond anvil cell, tracking its structure and texture by using time-resolved x-ray diffraction as the pressure increased to 200 GPa. The melting curve suggests the possibility of high heat flux and partial melting at the core-mantle boundary.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004053943851526","@type":"Researcher","foaf:name":[{"@value":"S. Anzellini"}],"jpcoar:affiliationName":[{"@value":"Commissariat à l’Énergie Atomique, Direction des Applications Militaires Île de France 91297 Arpajon Cedex, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843597540225","@type":"Researcher","foaf:name":[{"@value":"A. Dewaele"}],"jpcoar:affiliationName":[{"@value":"Commissariat à l’Énergie Atomique, Direction des Applications Militaires Île de France 91297 Arpajon Cedex, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843597540228","@type":"Researcher","foaf:name":[{"@value":"M. Mezouar"}],"jpcoar:affiliationName":[{"@value":"European Synchrotron Radiation Facility, BP 220, F-38043 Grenoble Cedex, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843597540226","@type":"Researcher","foaf:name":[{"@value":"P. Loubeyre"}],"jpcoar:affiliationName":[{"@value":"Commissariat à l’Énergie Atomique, Direction des Applications Militaires Île de France 91297 Arpajon Cedex, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843597540227","@type":"Researcher","foaf:name":[{"@value":"G. Morard"}],"jpcoar:affiliationName":[{"@value":"Institut de Minéralogie et de Physique des Milieux Condensés UMR CNRS 7590, Université Pierre et Marie Curie, 75005 Paris, France."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2013-04-26","prism:volume":"340","prism:number":"6131","prism:startingPage":"464","prism:endingPage":"466"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1233514"}],"createdAt":"2013-04-25","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213759428608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The effects of ferromagnetism and interstitial hydrogen on the 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