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author Zangalis, K P
Kharin, Gennady S
author_facet Zangalis, K P
Kharin, Gennady S
collection Datos científicos de ciencias marinas y ambientales
contents A comprehensive study of 102 samples of grain size fractions 0.010-0.005; 0.005-0.001, and <0.001 mm showns that clay mineral compositions from bottom sediments of the Faroe-Iceland Threshold and Faroe-Shetland Trench are different. In the first case it is essentially smectite-chlorite, in the second - mainly hydromicaceous. The difference in composition of clay minerals is due to influence of different source areas of terrigenous material.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_777092
institution PANGAEA
language en
publishDate 1977
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of <0.001 mm grain size fractions of bottom sediments and cementing mass of basalt breccia from the North Atlantic
Zangalis, K P
Kharin, Gennady S
38-337; Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Atlantic Ocean; Atomic absorption spectrometry (AAS); Cadmium; Calcium oxide; Calculated; Chromium; Copper; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; GC; Glomar Challenger; Grab; GRAB; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Leg38; Longitude of event; Loss on ignition; Magnesium oxide; Manganese oxide; Mikhail Lomonosov; ML26; ML26_2077GC; ML26_2080; ML26_2083-1; MULT; Multiple investigations; Nickel; North Atlantic/Norwegian Sea/BASIN; North Atlantic Ocean; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample type; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; Water in rock; Wet chemistry; Zinc
A comprehensive study of 102 samples of grain size fractions 0.010-0.005; 0.005-0.001, and <0.001 mm showns that clay mineral compositions from bottom sediments of the Faroe-Iceland Threshold and Faroe-Shetland Trench are different. In the first case it is essentially smectite-chlorite, in the second - mainly hydromicaceous. The difference in composition of clay minerals is due to influence of different source areas of terrigenous material.
title Chemical composition of <0.001 mm grain size fractions of bottom sediments and cementing mass of basalt breccia from the North Atlantic
topic 38-337; Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Atlantic Ocean; Atomic absorption spectrometry (AAS); Cadmium; Calcium oxide; Calculated; Chromium; Copper; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; GC; Glomar Challenger; Grab; GRAB; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Leg38; Longitude of event; Loss on ignition; Magnesium oxide; Manganese oxide; Mikhail Lomonosov; ML26; ML26_2077GC; ML26_2080; ML26_2083-1; MULT; Multiple investigations; Nickel; North Atlantic/Norwegian Sea/BASIN; North Atlantic Ocean; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample type; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; Water in rock; Wet chemistry; Zinc
url https://doi.org/10.1594/PANGAEA.777092