{"@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/1363670318288480512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1140855"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1140855"}},{"identifier":{"@type":"PMID","@value":"17556582"}}],"dc:title":[{"@value":"Seismic Evidence for Deep-Water Transportation in the Mantle"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            We report seismic evidence for the transportation of water into the deep mantle in the subduction zone beneath northeastern Japan. Our data indicate that water is released from the hydrated oceanic crust at shallow depths (<\n            <jats:sub>∼100</jats:sub>\n            kilometers) and then forms a channel of hydrated mantle material on top of the subducting plate that is the pathway for water into the deep mantle. Our result provides direct evidence that shows how water is transported from the ocean to the deep mantle in a cold subduction zone environment.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318288480512","@type":"Researcher","foaf:name":[{"@value":"Hitoshi Kawakatsu"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318288480513","@type":"Researcher","foaf:name":[{"@value":"Shingo Watada"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan."}]}],"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":"2007-06-08","prism:volume":"316","prism:number":"5830","prism:startingPage":"1468","prism:endingPage":"1471"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1140855"}],"createdAt":"2007-06-07","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202726472832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic evidence for thermally-controlled dehydration reaction in subducting oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1050298975368397568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3D thermal structural and dehydration modeling in the southern Chile subduction zone and its relationship to interplate earthquakes and the volcanic 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