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Screaton, Elizabeth J. et al. (2006): Permeabilities of Costa Rica subduction zone sediments
Leg/Site/Hole:
Related Expeditions:
ODP 205
Identifier:
ID:
2007-025140
Type:
georefid
ID:
10.2973/odp.proc.sr.205.204.2006
Type:
doi
Creator:
Name:
Screaton, Elizabeth J.
Affiliation:
University of Florida, Department of Geological Sciences, Gainesville, FL, United States
Role:
author
Name:
Hays, Troy
Affiliation:
Universitaet Bremen, Federal Republic of Germany
Role:
author
Name:
Gamage, Kusali
Affiliation:
Texas A&M University, United States
Role:
author
Name:
Martin, Jennifer
Affiliation:
Southampton Oceanography Centre, United Kingdom
Role:
author
Identification:
Title:
Permeabilities of Costa Rica subduction zone sediments
Year:
2006
Source:
In: Morris, Julie D., Villinger, Heinrich W., Klaus, Adam, Cardace, Dawn M., Chavagnac, Valerie M. C., Clift, Peter D., Haeckel, Matthias, Hisamitsu, Toshio, Kastner, Miriam, Pfender, Marion, Saffer, Demian M., Santelli, Cara, Schramm, Burkhard, Screaton, Elizabeth J., Solomon, Evan A., Strasser, Michael, Moe, Kyaw Thu, Vannucchi, Paola, Proceedings of the Ocean Drilling Program; scientific results; fluid flow and subduction fluxes across the Costa Rica convergent margin; implications for the seismogenic zone and subduction factory; covering Leg 205 of the cruises of the Drilling Vessel JOIDES Resolution; Victoria, Canada, to Balboa, Panama; Sites 1253-1255; 2 September-6 November 2002
Publisher:
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
Volume:
205
Issue:
Pages:
Abstract:
Constant-pressure difference and constant-flow permeability tests were conducted on core samples from Ocean Drilling Program Legs 170 and 205 from the Costa Rica subduction zone representing pelagic carbonate and hemipelagic mud lithologies. Seven whole-round core samples from Sites 1040, 1253, and 1255 were tested for vertical permeabilities. The permeabilities of the pelagic carbonate sediments range from approximately 4 X 10 (super -16) to approximately 1 X 10 (super -15) m (super 2) . The permeabilities of the hemipelagic mud sediments vary from approximately 2 X 10 (super -18) to approximately 4 X 10 (super -18) m (super 2) . To further characterize the sediments, grain size, total carbon, and total inorganic carbon analyses were conducted.
Language:
English
Genre:
Serial
Rights:
URL:
http://www-odp.tamu.edu/publications/205_SR/VOLUME/CHAPTERS/204.PDF
Coverage:
Geographic coordinates:
North:9.4000
West:-86.1200
East: -86.1000
South:9.3800
Keywords:
Oceanography; carbonate sediments; Central America; clastic sediments; Costa Rica; East Pacific; geochemistry; grain size; hemipelagic environment; inorganic materials; Leg 205; marine environment; marine sediments; Middle America Trench; mud; North Pacific; Northeast Pacific; Ocean Drilling Program; organic compounds; Pacific Ocean; pelagic environment; permeability; pressure; sediments; subduction zones; total organic carbon;
.
Copyright © 2006-2007 IODP-MI