{"data":{"id":"10.1594/pangaea.710841","type":"dois","attributes":{"doi":"10.1594/pangaea.710841","prefix":"10.1594","suffix":"pangaea.710841","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Gieskes, Joris M","givenName":"Joris M","familyName":"Gieskes","affiliation":[],"nameIdentifiers":[]},{"name":"Lawrence, James R","givenName":"James R","familyName":"Lawrence","affiliation":[],"nameIdentifiers":[]},{"name":"Galleisky, Guntwin","givenName":"Guntwin","familyName":"Galleisky","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Chemistry of interstitial water of samples from DSDP Leg 38"}],"publisher":"PANGAEA","container":{},"publicationYear":1976,"subjects":[{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"Composite Core","subjectScheme":"Method"},{"subject":"Leg38","subjectScheme":"Campaign"},{"subject":"Glomar Challenger","subjectScheme":"Basis"},{"subject":"Deep Sea Drilling Project (DSDP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1976","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":"10.2973/dsdp.proc.38394041s.112.1978","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["16 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":"Interstitial waters recovered during Leg 38 show large changes in major ion composition and also in oxygen isotope composition. Increases in Ca[++] and Sr[++] and decreases in K[+], Mg[++], and O18/O16 are interpreted in terms of extensive diagenesis of terrigenous, volcanic, or basaltic igneous materials in the sediments and underlying basalts. Slight, but well-established increases in chlorinity with depth indicate that these postulated weathering reactions involve uptake of water to a measurable extent. Interstitial waters from sites drilled on the Inner Voring Plateau suggest the infusion of fresh waters by aquifers from the mainland of Norway.","descriptionType":"Abstract"},{"description":"Supplement to: Gieskes, Joris M; Lawrence, James R; Galleisky, Guntwin (1976): Interstitial water studies, Leg 38. In: Talwani, M., Udintsev, G., et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Printing Office), 38, 121-133","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"7.8753","northBoundLatitude":"76.1497","southBoundLatitude":"37.949999999999996","westBoundLongitude":"-12.471"}},{"geoLocationPlace":"North Atlantic/Norwegian Sea"},{"geoLocationPlace":"North Atlantic/Norwegian Sea/BASIN"},{"geoLocationPlace":"North Atlantic/Norwegian Sea/PLATEAU"},{"geoLocationPlace":"North Atlantic/Norwegian Sea/DIAPIR"},{"geoLocationPlace":"North Atlantic/Greenland Sea/RIDGE"},{"geoLocationPlace":"North Atlantic/Norwegian Sea/RIDGE"},{"geoLocationPlace":"North 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