_version_ 1867170032182624256
author Faas, Richard W
author_facet Faas, Richard W
collection Datos científicos de ciencias marinas y ambientales
contents The plasticity characteristics of the Quaternary sediments of the Guatemalan continental margin were determined from five sites drilled during Leg 67 of the Deep Sea Drilling Project. The 64 samples analyzed are from various marine environments, including the Cocos Plate, Middle America Trench, and the trench lower slope to midslope of the Guatemalan continental slope. The sediments are primarily hemipelagic muds and trench-fill turbidites and include quantities of siliceous and calcareous biogenic components. The sediments are generally classified as organic clays of medium to high plasticity, containing micaceous sands and silts, with 14% classed as inorganic clays of medium to high plasticity. High sedimentation rates in Quaternary sediments are the result, in part, of sediment gravity flows that depend upon rheological properties, i.e., sediment plasticity. Mudflows and cohesive debris flows appear to be significant downslope transport mechanisms in these highly plastic sediments.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_817569
institution PANGAEA
language en
publishDate 1982
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Sediment properties at DSDP Leg 67 Holes
Faas, Richard W
67-494; 67-494A; 67-495; 67-496; 67-497; 67-499; Activity description; Atterberg limits test; Carbon, organic, total; Classification; Deep Sea Drilling Project; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Event label; Glomar Challenger; Grain size analysis after Atterberg; Latitude of event; Leg67; Liquidity index; Liquid limit; Longitude of event; North Pacific/SLOPE; North Pacific/TRENCH; Plastic index; Plastic limit; Ratio; Sample code/label; Sand; see reference(s); Silt; Size fraction < 0.002 mm, clay; Water content, dry mass
The plasticity characteristics of the Quaternary sediments of the Guatemalan continental margin were determined from five sites drilled during Leg 67 of the Deep Sea Drilling Project. The 64 samples analyzed are from various marine environments, including the Cocos Plate, Middle America Trench, and the trench lower slope to midslope of the Guatemalan continental slope. The sediments are primarily hemipelagic muds and trench-fill turbidites and include quantities of siliceous and calcareous biogenic components. The sediments are generally classified as organic clays of medium to high plasticity, containing micaceous sands and silts, with 14% classed as inorganic clays of medium to high plasticity. High sedimentation rates in Quaternary sediments are the result, in part, of sediment gravity flows that depend upon rheological properties, i.e., sediment plasticity. Mudflows and cohesive debris flows appear to be significant downslope transport mechanisms in these highly plastic sediments.
title (Table 1) Sediment properties at DSDP Leg 67 Holes
topic 67-494; 67-494A; 67-495; 67-496; 67-497; 67-499; Activity description; Atterberg limits test; Carbon, organic, total; Classification; Deep Sea Drilling Project; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Elevation of event; Event label; Glomar Challenger; Grain size analysis after Atterberg; Latitude of event; Leg67; Liquidity index; Liquid limit; Longitude of event; North Pacific/SLOPE; North Pacific/TRENCH; Plastic index; Plastic limit; Ratio; Sample code/label; Sand; see reference(s); Silt; Size fraction < 0.002 mm, clay; Water content, dry mass
url https://doi.org/10.1594/PANGAEA.817569