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Main Authors: Dadey, Kathleen A, Klaus, Adam
Format: Dataset Open Access
Language:en
Published: PANGAEA 1992
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Online Access:https://doi.org/10.1594/PANGAEA.774711
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author Dadey, Kathleen A
Klaus, Adam
author_facet Dadey, Kathleen A
Klaus, Adam
collection Datos científicos de ciencias marinas y ambientales
contents We examine the physical properties of volcaniclastic sediments in the forearc and backarc of the Izu-Bonin arc region. Based on our analyses of these and other deposits in the area, we conclude that, with the possible exception of pumice-rich material, unlithified volcaniclastics behave much like detrital deep-sea sediments. In contrast, lithified volcaniclastic sediments display unique physical properties, such as higher electrical resistivity and velocity than expected from porosity values. The primary cause of these phenomena is a lack of interconnectedness of the pore spaces and cementation of the volcaniclastic particles.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_774711
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle (Table 2) Consolidation characteristics of ODP Hole 126-790A samples
Dadey, Kathleen A
Klaus, Adam
126-790A; Compression index; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Euaugaptilus spp., copepodites, biomass as carbon; Joides Resolution; Leg126; Ocean Drilling Program; ODP; Overburden pressure; Overconsolidation ratio; Philippine Sea; Sample code/label
We examine the physical properties of volcaniclastic sediments in the forearc and backarc of the Izu-Bonin arc region. Based on our analyses of these and other deposits in the area, we conclude that, with the possible exception of pumice-rich material, unlithified volcaniclastics behave much like detrital deep-sea sediments. In contrast, lithified volcaniclastic sediments display unique physical properties, such as higher electrical resistivity and velocity than expected from porosity values. The primary cause of these phenomena is a lack of interconnectedness of the pore spaces and cementation of the volcaniclastic particles.
title (Table 2) Consolidation characteristics of ODP Hole 126-790A samples
topic 126-790A; Compression index; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Euaugaptilus spp., copepodites, biomass as carbon; Joides Resolution; Leg126; Ocean Drilling Program; ODP; Overburden pressure; Overconsolidation ratio; Philippine Sea; Sample code/label
url https://doi.org/10.1594/PANGAEA.774711