Proc. IODP, 307, Data report: dolomite in Neogene sediments of the Belgica carbonate mound province, Porcupine Seabight, North Atlantic

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Chapter contents Abstract Introduction Methods and materials Results Petrographic and X-ray diffraction analyses Distribution of dolomite SEM and electron probe analyses Geochemical analysis of interstitial waters Acknowledgments References Figures F1. Location maps. F2. Stratigraphic profile. F3. X-ray diffraction patterns. F4. Porcupine Basin sediments. F5. Schematic section. F6. Electron micrographs of dolomite. F7. Electron micrographs of dolomite. F8. Saturation index. PDF file			Previous \| Next doi:10.2204/iodp.proc.307.207.2009 References Budd, D.A., 1997. Cenozoic dolomites of carbonate islands: their attributes and origin. Earth-Sci. Rev., 42(1–2):1–47. doi:10.1016/S0012-8252(96)00051-7 De Mol, B., Van Rensbergen, P., Pillen, S., Van Herreweghe, K., Van Rooij, D., McDonnell, A., Huvenne, V., Ivanov, M., Swennen, R., and Henriet, J.-P., 2002. Large deep-water coral banks in the Porcupine Basin, southwest of Ireland. Mar. Geol., 188(1–2):193–231. doi:10.1016/S0025-3227(02)00281-5 Goldsmith, J.R., and Graf, D.L., 1958. Structural and compositional variations in some natural dolomites. J. Geol., 66:678–693. Gramling, C., 2006. Looking for geophysical signs of life. Geotimes, 51(11). http://www.geotimes.org/nov06/trends.html Gregg, J.M., Howard, S.A., and Mazzullo, S.J., 1992. Early diagenetic recrystallization of Holocene (<3000 years old) peritidal dolomites, Ambergris cay, Belize. Sedimentology, 39(1):143–160. doi:10.1111/j.1365-3091.1992.tb01027.x Gregg, J.M., Somerville, I.D., Foubert, A., and Doyle, E., 2006. Neogene deepwater carbonate mud-mounds and their Paleozoic counterparts—comparisons of geometry, sedimentology, and petrology. AAPG 2006 Annu. Conv.: Abstr. Vol., 15:40. Henriet, J.-P., Kano, A., Malone, M.J., and the Expedition 307 Project Team, 2005. Modern carbonate mounds: porcupine drilling. IODP Sci. Prosp., 307. doi:10.2204/iodp.sp.307.2005 Kano, A., Ferdelman, T.G., Williams, T., Henriet, J.-P., Ishikawa, T., Kawagoe, N., Takashima, C., Kakizaki, Y., Abe, K., Sakai, S., Browning, E.L., Li, X., and the Integrated Ocean Drilling Program Expedition 307 Scientists, 2007. Age constraints on the origin and growth history of a deep-water coral mound in the northeast Atlantic drilled during Integrated Ocean Drilling Program Expedition 307. Geology, 35(11):1051–1054. doi:10.1130/G23917A.1 Lees, A., and Miller, J., 1995. Waulsortian banks. In Monty, C.L.V., Bosence, D.W.J., Bridges, P.H., and Pratt, B.R. (Eds.), Carbonate Mud-Mounds: Their Origin and Evolution. Spec. Publ. Int. Assoc. Sedimentol., 23:191–271. Lumsden, D.N., and Chimahusky, J.S., 1980. Relationship between dolomite nonstoichiometry and carbonate facies parameters. In Zenger, D.H., Dunham, J.B., and Ethington, R.L. (Eds.), Concepts and Models of Dolomitization. Spec. Publ.—Soc. Econ. Paleontol. Mineral., 28:123–137. Machel, H.G., 1985. Cathodoluminescence in calcite and dolomite and its chemical interpretation. Geosci. Can., 12:139–147. Ntarlagiannis, D., Atekwana, E., Hill, E., and Gorby, Y., 2006. Bacterial nanowires facilitate electron transfer in saturated porous media. Eos, Trans. Am. Geophys. Union, 87(52)(Suppl.):NS21A-05. (Abstract) http://www.agu.org/meetings/fm06/waisfm06.html Top of page \| Previous \| Next

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