{"@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/1363670320081343744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1098/rspa.1954.0085"}},{"identifier":{"@type":"URI","@value":"https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1954.0085"}},{"identifier":{"@type":"URI","@value":"https://royalsocietypublishing.org/rspa/article-pdf/222/1150/408/48162/rspa.1954.0085.pdf"}}],"dc:title":[{"@value":"The flow of heat through the floor of the Atlantic Ocean"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>The measurement of the temperature gradient and thermal conductivity in the sediments beneath the floor of the North Atlantic Ocean is described. Measurements were made at five stations. The mean heat flow and conductivity were found to be 0·98 × 10-6 cal/cm2s and 25 × 10-4 cal/cm °Cs. The heat flows at the individual stations range from 0·58 to 1·42 × 10-6 cal/cm2s. The high heat flow is an unexpected result, and it is difficult to find a source for so much heat.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380025433875866112","@type":"Researcher","foaf:name":[{"@value":"Edward Crisp Bullard"}],"jpcoar:affiliationName":[{"@value":"National Physical Laboratory"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00804630"},{"@type":"EISSN","@value":"20539169"}],"prism:publicationName":[{"@value":"Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences"}],"dc:publisher":[{"@value":"The Royal Society"}],"prism:publicationDate":"1954-03-18","prism:volume":"222","prism:number":"1150","prism:startingPage":"408","prism:endingPage":"429"},"reviewed":"false","dc:rights":["https://royalsociety.org/journals/ethics-policies/data-sharing-mining/"],"url":[{"@id":"https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1954.0085"},{"@id":"https://royalsocietypublishing.org/rspa/article-pdf/222/1150/408/48162/rspa.1954.0085.pdf"}],"createdAt":"2006-12-15","modifiedAt":"2025-12-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050292726806574464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"In situ thermal excursions detected in the Nankai Trough forearc slope sediment at IODP NanTroSEIZE Site C0008"},{"@value":"In situ thermal excursions detected in Nankai Trough forearc slope sediment at IODP NanTroSEIZE Site C0008"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564289196820992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin"},{"@language":"en","@value":"Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088687104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismogenic zone temperatures and heat-flow anomalies in the To-nankai margin segment based on temperature data from IODP expedition 333 and thermal model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092378026752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Expedition 379 methods"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891990481024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Constraints on the fluid supply rate into and through gas hydrate reservoir systems as inferred from pore-water chloride and in situ temperature profiles, Krishna-Godavari Basin, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680293655552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heat flow distribution on the floor of Nankai Trough off Kumano and implications for the geothermal regime of subducting sediments"},{"@value":"Heat flow on the Nankai Trough off Kumano"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1098/rspa.1954.0085"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0171-1_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.06.048_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"},{"@type":"CROSSREF","@value":"10.1029/2012gc004260_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"},{"@type":"CROSSREF","@value":"10.14379/iodp.proc.379.102.2021_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"},{"@type":"CROSSREF","@value":"10.1016/j.marpetgeo.2018.12.049_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.8.13_references_DOI_X2tsHQvM6EmBKOyeLp1oW1w9nWm"}]}