{"data":{"id":"10.1594/pangaea.708737","type":"dois","attributes":{"doi":"10.1594/pangaea.708737","prefix":"10.1594","suffix":"pangaea.708737","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Dietrich, Volker","givenName":"Volker","familyName":"Dietrich","affiliation":[],"nameIdentifiers":[]},{"name":"Emmermann, Rolf","givenName":"Rolf","familyName":"Emmermann","affiliation":[],"nameIdentifiers":[]},{"name":"Keller, Jörg","givenName":"Jörg","familyName":"Keller","affiliation":[],"nameIdentifiers":[]},{"name":"Puchelt, Harald","givenName":"Harald","familyName":"Puchelt","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Geochemistry of the basalts from DSDP Leg 42A"}],"publisher":"PANGAEA","container":{},"publicationYear":1977,"subjects":[{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"Leg42","subjectScheme":"Campaign"},{"subject":"Glomar Challenger","subjectScheme":"Basis"},{"subject":"Deep Sea Drilling Project (DSDP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1975-04-27T00:00:00","dateType":"Collected"},{"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)90211-4","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":"During DSDP Leg 42A, drilling at site 373A in the central Tyrrhenian Sea penetrated Miocene basaltic basement for 190 m and recovered basalt from up to 450 m below the sea floor. Despite mineralogical and chemical alteration due to hydrothermal processes under the high heat flow regime in the Tyrrhenian marginal basin, petrological analogies to high-Al abyssal basalts can be traced. Two interlayered basalt groups have been recognized: (1) the lower-Ti group (core 5/1-2, core 7, 10), and (2) the higher-Ti group (core 5/3, core 6, core 11, core 12 and outer barrel), respectively. We consider a distinction of two magma types: a more primitive magma leading to the plagioclase-bearing, lower-Ti basalts with affinities to high-Al abyssal tholeiites and a more differentiated magma leading to basalts with higher Ti.","descriptionType":"Abstract"},{"description":"Supplement to: Dietrich, Volker; Emmermann, Rolf; Keller, Jörg; Puchelt, Harald (1977): Tholeiitic basalts from the Tyrrhenian sea floor. Earth and Planetary Science Letters, (36(2), 285-296","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"39.728","pointLongitude":"12.9927"}},{"geoLocationPlace":"Mediterranean 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