Permeabilities, grain size and carbon composition of sediments from ODP Hole 170-1040C and two Leg 205 holes

DOI

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 ~4 x 10-16 to ~1 x 10-15 m2. The permeabilities of the hemipelagic mud sediments vary from ~2 x 10-18 to ~4 x 10-18 m2. To further characterize the sediments, grain size, total carbon, and total inorganic carbon analyses were conducted.

Supplement to: Screaton, Elizabeth J; Hays, Troy; Gamage, Kusali; Martin, Jennifer (2006): Data report: Permeabilities of Costa Rica subduction zone sediments. In: Morris, JD; Villinger, HW; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 205, 1-13

Identifier
DOI https://doi.org/10.1594/PANGAEA.775480
Related Identifier IsSupplementTo https://doi.org/10.2973/odp.proc.sr.205.204.2006
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.775480
Provenance
Creator Screaton, Elizabeth J; Hays, Troy; Gamage, Kusali; Martin, Jennifer
Publisher PANGAEA
Publication Year 2006
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (-86.191W, 9.648S, -86.179E, 9.662N); Costa Rica subduction complex, North Pacific Ocean; North Pacific Ocean
Temporal Coverage Begin 1996-11-11T05:30:00Z
Temporal Coverage End 2002-10-26T00:00:00Z