{"data":{"id":"10.1594/pangaea.715064","type":"dois","attributes":{"doi":"10.1594/pangaea.715064","prefix":"10.1594","suffix":"pangaea.715064","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"MacDougall, J Douglas","givenName":"J Douglas","familyName":"MacDougall","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Uranium in marine basalts"}],"publisher":"PANGAEA","container":{},"publicationYear":1977,"subjects":[{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"Leg2","subjectScheme":"Campaign"},{"subject":"Leg5","subjectScheme":"Campaign"},{"subject":"Leg16","subjectScheme":"Campaign"},{"subject":"Leg18","subjectScheme":"Campaign"},{"subject":"Leg22","subjectScheme":"Campaign"},{"subject":"Leg23","subjectScheme":"Campaign"},{"subject":"Leg24","subjectScheme":"Campaign"},{"subject":"Leg25","subjectScheme":"Campaign"},{"subject":"Leg34","subjectScheme":"Campaign"},{"subject":"Glomar Challenger","subjectScheme":"Basis"},{"subject":"Deep Sea Drilling Project (DSDP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1977","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1016/0012-821x(77)90029-2","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["2 datasets"],"formats":["application/zip"],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 3.0 Unported","rightsUri":"https://creativecommons.org/licenses/by/3.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-3.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"The uranium content of glass from chilled margins of oceanic tholeiitic basalt flows is generally \u0026lt;0.1 ppm, even for old samples with highly altered crystalline interiors. Such low values represent the original whole rock concentrations, although subsequent to eruption low-temperature weathering has added uranium, and other elements, to the crystalline portions of these basalts. Consideration of the K/U ratios of altered samples suggests that basalt weathering may provide the major oceanic sink for these two elements.","descriptionType":"Abstract"},{"description":"Supplement to: MacDougall, J Douglas (1977): Uranium in marine basalts: Concentration, distribution and implications. Earth and Planetary Science Letters, 35(1), 65-70","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"-22.837649999999996","northBoundLatitude":"50.4697","southBoundLatitude":"-13.0173","westBoundLongitude":"93.8962"}},{"geoLocationPlace":"North Atlantic/CONT RISE"},{"geoLocationPlace":"North Pacific/PLAIN"},{"geoLocationPlace":"North Pacific/RIDGE"},{"geoLocationPlace":"North Pacific/HILL"},{"geoLocationPlace":"North Pacific/CONT RISE"},{"geoLocationPlace":"Indian Ocean//BASIN"},{"geoLocationPlace":"Indian Ocean/Arabian Sea/HILL"},{"geoLocationPlace":"Indian Ocean/Gulf of Aden/BASIN"},{"geoLocationPlace":"Indian Ocean//FRACTURE ZONE"},{"geoLocationPlace":"South 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