georefid:2005-041670georefid:2005-041660SEDIS 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.182.010.2002<gco:CharacterString>Carbonate mineralogy of sites drilled during Leg 182</gco:CharacterString>2004-01-01publicationgeorefid:2005-041670doi:10.2973/odp.proc.sr.182.010.2002Swart, Peter K.University of Miami, Rosenstiel School of Marine and Atmospheric Science, Miami, FL, United StatesauthorJames, Noel P.Australian Geological Survey Organisation, AustraliaauthorMallinson, DavidTexas A&M University, United StatesauthorMalone, Mitchell J.Eidgenoessische Technische Hochschule-Zentrum, SwitzerlandauthorMatsuda, HirokiJohann Wolfgang Goethe-Universitaet, Federal Republic of GermanyauthorSimo, ToniEckerd College, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Hine, Albert C., Feary, David A., Malone, Mitchell J., Andres, Miriam, Betzler, Christian, Brooks, Gregg R., Brunner, Charlotte A., Fuller, Michael, Molina Garza, Roberto S., Holbourn, Ann E., Huuse, Mads, Isern, Alexandra R., James, Noel P., Ladner, Bryan C., Li, Qianyu, Machiyama, Hideaki, Mallinson, David J., Matsuda, Hiroki, Mitterer, Richard M., Robin, Cecile, Russell, Joellen L., Shafik, Samir, Simo, J. A., Smart, Peter L., Spence, Guy H., Surlyk, Finn C., Swart, Peter K., Wortmann, Ulrich G., Proceedings of the Ocean Drilling Program; scientific results; Great Australian Bight; Cenozoic cool-water carbonates; covering Leg 182 of the cruises of the drilling vessel JOIDES Resolution; Wellington, New Zealand, to Fremantle, Australia; Sites 1126-1134, 8 October-7 December 1998182Carbonate mineralogy was determined on a total of 2845 samples from Sites 1126-1132 situated on the southern margin of the Australian continent. Five of these sites represent distal to proximal transects (Sites 1127-1131-1129 and 1132-1130), which penetrate principally Pleistocene-aged sediments. These sediments exhibit high concentrations of aragonite and high-Mg calcite (HMC) in shallow portions of the core, decreasing with depth. Dolomite was ubiquitous throughout these five cores and showed an inverse correlation in some instances with HMC. Sites 1126 and 1128 penetrated older strata and show lower concentrations of aragonite, HMC, and dolomite.completedOceanographyaragoniteAustralasiaAustraliacalcitecarbonate sedimentscarbonatesCenozoicconcentrationcoresdolomiteGreat Australian BightIndian OceanLeg 182marine sedimentsmineral compositionOcean Drilling Programocean floorssedimentsX-ray diffraction dataurn:org.iodp:exp:182urnlargerWorkCitationcampaignEnglishgeoscientificInformation127.1500128.5500-34.2330-33.1720Available 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/182_SR/VOLUME/CHAPTERS/010.PDFdownload