georefid:2004-019654SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2004-0196542001-01-01publicationgeorefid:2004-019654Forsberg, Carl F.Norwegian Polar Institute Polarmiljosenteret, Tromso, NorwayauthorSolheim, AndersNorwegian Geotechnical Institute, NorwayauthorGruetzner, JensUniversitaet Bremen, Federal Republic of GermanyauthorTaylor, BrianJacques Whitford & Associates, CanadaauthorStrand, KariUniversity of Oulu, FinlandauthorIstituto Nazionale di Geofisica e Vulcanologia, Rome, ItalypublisherdocumentHardcopyIn: Florindo, Fabio (editor), Cooper, Alan K. (editor), Extended abstracts for the International ANTOSTRAT symposium on The geologic record of the Antarctic ice sheet from drilling, coring and seismic studies1671-72ODP sites 1166 and 1167, Antarctic continental margin in the Prydz Bay sector of the Southern Ocean, provide evidence for studying the glacial growth on Antarctica during the Eocene-Oligocene transition. Site 1167 provides good evidence of sedimentation associated with movement of the Antarctic ice sheet. This study looks at the mineralogical and geotechnical properties that control the lithostratigraphy as a way to understand the glacial evolution of the Prydz Bay region. (MTE)completedStratigraphyAntarcticaCenozoicclay mineralscontinental marginEoceneglacial environmentglaciationglaciomarine environmentgrain sizeLeg 188lithofaciesmarine environmentmechanical propertiesmineral compositionOcean Drilling ProgramODP Site 1166ODP Site 1167OligocenePaleogenePrydz Bayresistivitysheet silicatessilicatessize distributionSouthern OceanTertiaryurn:org.iodp:exp:188urnlargerWorkCitationcampaignurn:org.iodp:exp:188:site:1166urnlargerWorkCitationstudyurn:org.iodp:exp:188urnlargerWorkCitationcampaignurn:org.iodp:exp:188:site:1167urnlargerWorkCitationstudyurn:org.iodp:exp:188urnlargerWorkCitationcampaignEnglishgeoscientificInformation72.170074.4800-67.4200-66.2400