{"@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/1361981469461576832.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2011.01.004"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X11000161?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X11000161?httpAccept=text/plain"}}],"dc:title":[{"@value":"Mantle P-wave velocity structure beneath the Hawaiian hotspot"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469461576834","@type":"Researcher","foaf:name":[{"@value":"Cecily J. Wolfe"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576837","@type":"Researcher","foaf:name":[{"@value":"Sean C. Solomon"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576704","@type":"Researcher","foaf:name":[{"@value":"Gabi Laske"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576835","@type":"Researcher","foaf:name":[{"@value":"John A. Collins"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576705","@type":"Researcher","foaf:name":[{"@value":"Robert S. Detrick"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576836","@type":"Researcher","foaf:name":[{"@value":"John A. Orcutt"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576833","@type":"Researcher","foaf:name":[{"@value":"David Bercovici"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469461576832","@type":"Researcher","foaf:name":[{"@value":"Erik H. Hauri"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-03","prism:volume":"303","prism:number":"3-4","prism:startingPage":"267","prism:endingPage":"280"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X11000161?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X11000161?httpAccept=text/plain"}],"createdAt":"2011-02-06","modifiedAt":"2018-12-05","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215942218752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isotopic heterogeneity of oceanic, arc and continental basalts and its implications for mantle dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186250366336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Broadband Ocean-Bottom Seismology"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791867589504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of shallow-layer reverberation on measurement of teleseismic P-wave travel times for ocean bottom seismograph data"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.01.004"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0626-2_references_DOI_YurTk1dtK7kkmZ87UvRVfx0cha5"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2014.09.003_references_DOI_YurTk1dtK7kkmZ87UvRVfx0cha5"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-060313-054818_references_DOI_YurTk1dtK7kkmZ87UvRVfx0cha5"}]}