Consolidation characteristics and permeabilities of sediments from the Japan Sea

Fuente: PANGAEA
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Autor principal: Holler, Peter R
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1992
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author Holler, Peter R
author_facet Holler, Peter R
collection Datos científicos de ciencias marinas y ambientales
contents The results of laboratory consolidation tests and undrained shear strength determinations of sediments from the Oki Ridge and the Kita Yamato Trough show that the sediments are overconsolidated to normally consolidated to a depth of about 20 m below the seafloor. Below that depth, the sediments are highly underconsolidated, implying high excess pore-water pressures. The most probable mechanism for the generation of the excess pore-water pressure is gas in sediments.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_778219
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle Consolidation characteristics and permeabilities of sediments from the Japan Sea
Holler, Peter R
128-798B; 128-799A; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg128; Ocean Drilling Program; ODP
The results of laboratory consolidation tests and undrained shear strength determinations of sediments from the Oki Ridge and the Kita Yamato Trough show that the sediments are overconsolidated to normally consolidated to a depth of about 20 m below the seafloor. Below that depth, the sediments are highly underconsolidated, implying high excess pore-water pressures. The most probable mechanism for the generation of the excess pore-water pressure is gas in sediments.
title Consolidation characteristics and permeabilities of sediments from the Japan Sea
topic 128-798B; 128-799A; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg128; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.778219