{"@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/1362262945824329728.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.aag3055"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.aag3055"}}],"dc:title":[{"@value":"Vertically extensive and unstable magmatic systems: A unified view of igneous processes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Making magma chambers from mush</jats:title>\n          <jats:p>\n            Shallow magma chambers either erupt as volcanoes or solidify as intrusive magma bodies. These magma bodies are traditionally considered to be long-lived and dominated by melt. Cashman\n            <jats:italic>et al.</jats:italic>\n            review the evidence that shallow magma chambers are actually assembled quickly from much larger, crystal-rich transcrustal magmatic systems. This paradigm helps explain many geophysical and geochemical features of volcanic systems. It also presents challenges for understanding the evolution of magma and provides insight into how and why volcanoes erupt.\n          </jats:p>\n          <jats:p>\n            <jats:italic>Science</jats:italic>\n            , this issue p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6331\" page=\"eaag3055\" related-article-type=\"in-this-issue\" vol=\"355\" xlink:href=\"10.1126/science.aag3055\">eaag3055</jats:related-article>\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262945824329728","@type":"Researcher","foaf:name":[{"@value":"Katharine V. Cashman"}],"jpcoar:affiliationName":[{"@value":"School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945824329729","@type":"Researcher","foaf:name":[{"@value":"R. Stephen J. Sparks"}],"jpcoar:affiliationName":[{"@value":"School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945824329730","@type":"Researcher","foaf:name":[{"@value":"Jonathan D. Blundy"}],"jpcoar:affiliationName":[{"@value":"School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK."}]}],"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":"2017-03-24","prism:volume":"355","prism:number":"6331","prism:startingPage":"eaag3055"},"reviewed":"false","dc:rights":["http://www.sciencemag.org/about/science-licenses-journal-article-reuse"],"url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.aag3055"}],"createdAt":"2017-03-23","modifiedAt":"2024-01-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338872851456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magmatic inflation in 2008–2010 at Mt. 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