georefid:2004-019666SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2004-019666<gco:CharacterString>Late Miocene to Quaternary deposition of biogenic opal and clay minerals on the continental rise west of the Antarctic Peninsula</gco:CharacterString>2001-01-01publicationgeorefid:2004-019666Hillenbrand, Claus-DieterAlfred Wegener Institute for Polar and Marine Research, Bremerhaven, Federal Republic of GermanyauthorFuetterer, Dieter K.University of Leipzig, Federal Republic of GermanyauthorEhrmann, WernerauthorIstituto 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 studies1699Neogene to Quaternary records of marine sediments were collected from ODP sites 1095 and 1096, continental rise in the Pacific sector of the Southern Ocean off the Antarctic Peninsula. Biogenic opal and clay minerals of the sediment drift are studied. (MTE)completedStratigraphyAntarctic PeninsulaAntarcticabiogenic processesCenozoicclay mineralscontinental riseframework silicatesglacial environmentLeg 178lithofaciesmarine environmentmarine transportOcean Drilling Programocean floorsODP Site 1095ODP Site 1096opalsediment transportsheet silicatessilica mineralssilicatesSouthern Oceanterrigenous materialsurn:org.iodp:exp:178urnlargerWorkCitationcampaignurn:org.iodp:exp:178:site:1095urnlargerWorkCitationstudyurn:org.iodp:exp:178urnlargerWorkCitationcampaignurn:org.iodp:exp:178:site:1096urnlargerWorkCitationstudyurn:org.iodp:exp:178urnlargerWorkCitationcampaignEnglishgeoscientificInformation-78.2916-76.5749-67.3401-66.5907