{"@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/1363388844839844864.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1174156"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1174156"}}],"dc:title":[{"@value":"Water and the Oxidation State of Subduction Zone Magmas"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Tracing Mantle Oxidation</jats:title>\n          <jats:p>\n            The chemical composition of the Earth's mantle varies with tectonic setting. For example, basaltic melts near subduction zones are more oxidized than magma near divergent plate boundaries.\n            <jats:bold>Kelley and Cottrell</jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"605\" related-article-type=\"in-this-issue\" vol=\"325\" xlink:href=\"10.1126/science.1174156\">605</jats:related-article>\n            ; see the Perspective by\n            <jats:bold>\n              <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"5940\" page=\"545\" related-article-type=\"in-this-issue\" vol=\"325\" xlink:href=\"10.1126/science.1176882\">Hirschmann</jats:related-article>\n            </jats:bold>\n            ) examined melts formed in different tectonic environments, using highly sensitive synchrotron-based analytical methods. The oxidation state of Fe increased with water content and mobile trace elements concentrations. Thus, fluids released from wet subducting plates drive mantle oxidation above subduction zones, which may help to explain the spatial differences in oxygen fugacity of the mantle.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844839844865","@type":"Researcher","foaf:name":[{"@value":"Katherine A. Kelley"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844839844864","@type":"Researcher","foaf:name":[{"@value":"Elizabeth Cottrell"}],"jpcoar:affiliationName":[{"@value":"National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00368075"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2009-07-31","prism:volume":"325","prism:number":"5940","prism:startingPage":"605","prism:endingPage":"607"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1174156"}],"createdAt":"2009-11-06","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216807252224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002217652601088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting of the Uppermost Metasomatized Asthenosphere Triggered by Fluid Fluxing from Ancient Subducted Sediment: Constraints from the Quaternary Basalt Lavas at Chugaryeong Volcano, 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