Teichert, Barbara M. A. and Bohrmann, Gerhard (2005): Composition of authigenic carbonates in sediments of the Cascadia accretionary prism, ODP Leg 204

Leg/Site/Hole:
ODP 204
Identifier:
2007-035093
georefid

10.2973/odp.proc.sr.204.116.2006
doi

Creator:
Teichert, Barbara M. A.
Bundesanstalt fuer Geowissenschaften und Rohstoffe, Hanover, Federal Republic of Germany
author

Bohrmann, Gerhard
Christian-Albrechts-Universitaet zu Kiel, Federal Republic of Germany
author

Identification:
Composition of authigenic carbonates in sediments of the Cascadia accretionary prism, ODP Leg 204
2005
In: Trehu, Anne M., Bohrmann, Gerhard, Torres, Marta E., Rack, Frank R., Bangs, Nathan L., Barr, Samantha R., Borowski, Walter S., Claypool, George E., Collett, Timothy S., Delwiche, Mark E., Dickens, Gerald R., Goldberg, David S., Gracia, Eulalia, Guerin, Gilles, Holland, Melanie, Johnson, Joel E., Lee, Young-Joo, Liu, Char-Shine, Long, Philip E., Milkov, Alexei V., Riedel, Michael, Schultheiss, Peter, Su Xin, Teichert, Barbara, Tomaru, Hitoshi, Vanneste, Maarten, Watanabe, Mahito, Weinberger, Jill L., Boetius, Antje, Brockman, Fred J., Deyhle, Annette, Fehn, Udo, Flemings, Peter B., Girguis, Peter R., Heesemann, Martin, Joye, Samantha B., Lorenson, Thomas D., Mills, Christopher T., Musgrave, Robert J., Popa, Radu, Ussler, Bill, Wilkes, Heinz, Winckler, Gisela, Winters, William J., Proceedings of the Ocean Drilling Program; scientific results; drilling gas hydrates on Hydrate Ridge, Cascadia continental margin; covering Leg 204 of the cruises of the drilling vessel JOIDES Resolution; Victoria, British Columbia, Canada, to Victoria, British Columbia, Canada; Sites 1244-1252; 7 July-2 September 2002
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
204
Carbonate mineralogy and carbonate content were determined on 65 samples from Sites 1244-1252, which were drilled on southern Hydrate Ridge and in an adjacent slope basin at the Cascadia accretionary prism. X-ray diffraction analyses data indicate varying carbonate compositions. Pure calcites are rare but were found at Sites 1246 and 1252. Low- and high-magnesium calcites are the dominant carbonate mineralogies and occur at all sites. The presence of dolomite is characteristic for the slope basin sites. The sampling depth of the carbonates varies from near seafloor to deep within the accretionary complex, suggesting different modes of carbonate formation. The summit, flank, and slope basin sites show characteristic carbonate compositions with different carbonate contents in distinct depth intervals.
English
Coverage:Geographic coordinates:
North:44.3500
West:-125.0900East: -125.0400
South:44.3400

Oceanography; Mineralogy of non-silicates; accretionary wedges; authigenic minerals; carbonates; Cascadia subduction zone; dolomite; East Pacific; geochemistry; Hydrate Ridge; Leg 204; marine sediments; North Pacific; Northeast Pacific; Ocean Drilling Program; ocean floors; Pacific Ocean; sediments; X-ray diffraction data;

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