{"data":{"id":"10.1594/pangaea.510769","type":"dois","attributes":{"doi":"10.1594/pangaea.510769","prefix":"10.1594","suffix":"pangaea.510769","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Sandroni, Sonja","givenName":"Sonja","familyName":"Sandroni","affiliation":[],"nameIdentifiers":[]},{"name":"Talarico, Franco M","givenName":"Franco M","familyName":"Talarico","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0002-7254-4301","nameIdentifierScheme":"ORCID"}],"affiliation":[]}],"titles":[{"title":"Geochemistry of basement clasts from sediment core CRP-3 in the ross Sea, Antarctica"}],"publisher":"PANGAEA","container":{},"publicationYear":2001,"subjects":[{"subject":"Core wireline system","subjectScheme":"Method"},{"subject":"CRP-3__Campaign","subjectScheme":"Campaign"},{"subject":"Sampling/drilling from ice","subjectScheme":"Basis"},{"subject":"Cape Roberts Project (CRP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"2001","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":"10013/epic.28227.d001","relatedIdentifierType":"Handle"}],"relatedItems":[],"sizes":["3 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":"Distribution patterns and petrographical and mineral chemistry data are described for the most representative basement lithologies occuring as clast in the c. 824 m thick Tertiary sedimentary sequence at the CRP-3 drillsite. These are granule to bolder grain size clasts of igneous and metamorphic rocks. Within the basement clast assemblage, granitoid pebbles are the predominant lithology. They consist of dominant grey biotic-bearing monzogranite, pink biotite-hornblende monzogranite, and biotite-bearing leucomomonzgranite. Minor lithologies include: actinolite-bearing leucotonalite, microgranite, biotite-hornblende quartz-monzonitic porphyr, and foliated biotic leucomonzogranite. Metamorphic clasts include rocks of both granitic and sedimentary derivation. They include mylonitic biotic orthogneiss, with or without garnet, muscovite-bearing quartzite, sillimanite-biotite paragneiss, biotite meta-sandstone, biotite-spotted schist, biotite-clacite-clinoamphibole meta-feldspathic arenite, biotite-calcite-clinozoisite meta-siltstone, biotite±clinoamphibole meta-marl, and graphite-bearing marble. As in previous CRP drillcores, the ubiquitous occurence of biotite±hornblende monzogranite pebbles is indicative of a local provenance, closely mirroring the dominance of these lithologies in the on-shore basement, where the Cambro-Ordovician Granite Harbour Intrusive Complex forms the most extensively exposed rock unit.","descriptionType":"Abstract"},{"description":"Supplement to: Sandroni, Sonja; Talarico, Franco M (2001): Petrography and provenance of basement clasts and clast variability in CRP-3 drillcore (Victoria Land Basin, Antarctica). http://www.mna.unisi.it/english/Publications/TAP/TA_pdfs/Volume_08/CRP3_Science_Results/TA_08_449_Sandroni.pdf, Terra Antartica, 8(4), 449-468","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":-77.006,"pointLongitude":163.71900000000002}},{"geoLocationPlace":"Ross 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