Knoop, Peter A. (2006): Inorganic geochemistry of hydrothermal sediments, Hole 1215A

Leg/Site/Hole:
ODP 199
ODP 199 1215
Identifier:
2007-028671
georefid

10.2973/odp.proc.sr.199.218.2006
doi

Creator:
Knoop, Peter A.
University of Michigan, School of Information, Ann Arbor, MI, United States
author

Identification:
Inorganic geochemistry of hydrothermal sediments, Hole 1215A
2006
In: Wilson, Paul A., Lyle, Mitchell W., Janecek, Thomas R., Backman, Jan, Busch, William H., Coxall, Helen K., Faul, Kristina, Gaillot, Philippe, Hovan, Steven A., Knoop, Peter, Kruse, Silke, Lanci, Luca, Lear, Caroline, Moore, Theodore C., Nigrini, Catherine A., Nishi, Hiroshi, Nomura, Ritsuo, Norris, Richard D., Palike, Heiko, Pares, Josep M., Quintin, Lacie, Raffi, Isabella, Rea, Brice R., Steiger, Torsten H., Tripati, Aradhna, Vanden Berg, Michael D., Wade, Bridget, Proceedings of the Ocean Drilling Program; scientific results; Paleogene equatorial transect; covering Leg 199 of the cruises of the drilling vessel JOIDES Resolution; Honolulu, Hawaii, to Honolulu, Hawaii; Sites 1215-1222; 23 October-16 December 2001
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
199
Elemental concentrations were determined on 21 samples from Hole 1215A to evaluate the influence of hydrothermal sources on bulk sediment composition. Rare earth element (REE) concentrations were also determined on 10 of these samples. Concentration profiles and REE patterns are consistent with a strong hydrothermal influence on sediment composition at the base of Hole 1215A.
English
Serial
Coverage:Geographic coordinates:
North:26.0200
West:-147.5600East: -147.5600
South:26.0200

Geochemistry of rocks, soils, and sediments; Oceanography; chemical composition; concentration; cores; Equatorial Pacific; geochemical cycle; geochemistry; hydrothermal conditions; inorganic materials; Leg 199; marine sediments; metals; Ocean Drilling Program; ODP Site 1215; Pacific Ocean; rare earths; sediments;

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