georefid:2005-011457georefid:2005-011446SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.sr.189.114.2004<gco:CharacterString>Bulk and clay mineral assemblages of the Tasmanian area, Maastrichtian-Pleistocene, ODP Leg 189</gco:CharacterString>2004-01-01publicationgeorefid:2005-011457doi:10.2973/odp.proc.sr.189.114.2004Robert, Christian M.Centre d'Oceanologie de Marseille, Marseilles, FranceauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Exon, Neville F., Kennett, James P., Malone, Mitchell J., Brinkhuis, Henk, Chaproniere, George C. H., Ennyu, Atsuhito, Fothergill, Patrick, Fuller, Michael D., Grauert, Marianne, Hill, Peter J., Janecek, Thomas R., Kelly, Daniel C., Latimer, Jennifer C., Nees, Stefan, Ninnemann, Ulysses S., Nuernberg, Dirk, Pekar, Stephen F., Pellaton, Caroline C., Pfuhl, Helen A., Robert, Christian M., Roessig, Kristeen L. McGonigal, Roehl, Ursula, Schellenberg, Stephen A., Shevenell, Amelia E., Stickley, Catherine E., Suzuki, Noritoshi, Touchard, Yannick, Wei, Wuchang, White, Timothy S., Proceedings of the Ocean Drilling Program; scientific results; the Tasmanian gateway; Cenozoic climatic and oceanographic development; covering Leg 189 of the cruises of the drilling vessel JOIDES Resolution; Hobart, Tasmania, to Sydney, Australia; Sites 1168-1172; 11 March-6 May 2000189Bulk and clay mineral investigations were conducted on approximately 750 samples from four sites drilled during Ocean Drilling Program Leg 189 on the western Tasmanian margin (Site 1168), the South Tasman Rise (Sites 1170 and 1171), and the East Tasman Plateau (Site 1172). The mineralogy of the bulk sediment is very similar at all sites, and major changes coincide with the boundaries of the three main lithologic units described in the Leg 189 Initial Reports volume. The clay mineral assemblages show significant regional differences, but their major variations coincide at all sites and with major changes in regional tectonics and climate.completedStratigraphyAntarctic ice sheetAntarcticaassemblagesCenozoicclay mineralogyclay mineralsclimate changecoresCretaceousdepositional environmentice sheetsIndian OceanLeg 189lithostratigraphyMaestrichtianMesozoicOcean Drilling Programocean floorsODP Site 1168ODP Site 1170ODP Site 1171ODP Site 1172Pacific OceanpaleoclimatologypaleogeographyPleistoceneQuaternaryreconstructionSenoniansheet silicatessilicatesSouth PacificSouthwest PacificTasman SeaUpper CretaceousWest Pacificurn:org.iodp:exp:189urnlargerWorkCitationcampaignurn:org.iodp:exp:189:site:1168urnlargerWorkCitationstudyurn:org.iodp:exp:189urnlargerWorkCitationcampaignurn:org.iodp:exp:189:site:1170urnlargerWorkCitationstudyurn:org.iodp:exp:189urnlargerWorkCitationcampaignurn:org.iodp:exp:189:site:1171urnlargerWorkCitationstudyurn:org.iodp:exp:189urnlargerWorkCitationcampaignurn:org.iodp:exp:189:site:1172urnlargerWorkCitationstudyurn:org.iodp:exp:189urnlargerWorkCitationcampaignEnglishgeoscientificInformation144.0000150.0000-48.3000-42.3000Available only on CD-ROM in PDF format and on the Web in PDF or HTML; data reportapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www-odp.tamu.edu/publications/189_SR/VOLUME/CHAPTERS/114.PDFdownload