georefid:1999-011792SEDIS 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=1999-0117921998-01-01publicationgeorefid:1999-011792Swart, Peter K.Rosenstiel School of Marine and Atmospheric Sciences, Marine Geology and Geophysics, Miami, FL, United StatesauthorMelim, LeslieWestern Illinois University, United StatesauthorEberli, GregorauthorAmerican Association of Petroleum Geologists and Society of Economic Paleontologists and Mineralogists, Tulsa, OK, United StatespublisherdocumentHardcopyIn: Anonymous, American Association of Petroleum Geologists 1998 annual meeting1998The processes of dissolution and cementation, which have been documented in the sub-surface of modern and ancient carbonate platforms, are being driven by the oxidation of organic material in marine dominated fluids. The influence of these processes are not restricted only to the margins of the platform as waters are being circulated as a result of temperature differences between the interior and the adjacent seaway. This circulation of water not only distributes the corrosive waters to other regions of the platform promoting extensive carbonate diagenesis, but also provides a mechanism for the continual supply of sulfate which oxidizes autochthonous organic material and thermogenically derived hydrocarbons.completedEconomic geology, geology of energy sourcesSedimentary petrologyAtlantic OceanC-13/C-12carboncarbon dioxidecarbonate platformscarbonatescementationcorediagenesisfabricGreat Bahama Bankhydrogen sulfideisotope ratiosisotopesLeg 166magnesian calcitemeteoric watermigrationNorth AtlanticO-18/O-16Ocean Drilling Programorganic compoundsoxidationoxygenpetroleumprocessesrecrystallizationsolutionstable isotopesurn:org.iodp:exp:166urnlargerWorkCitationcampaignEnglishgeoscientificInformation-79.2800-76.000022.000026.0000Great Bahama Bank