(Table 1) Chemical composition of ethmodiscus oozes from the Indian Ocean

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1. Verfasser: Sval'nov, Vyacheslav N
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Sprache:en
Veröffentlicht: PANGAEA 1974
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author Sval'nov, Vyacheslav N
author_facet Sval'nov, Vyacheslav N
collection Datos científicos de ciencias marinas y ambientales
contents A study was made of mineral composition of sand- and silt-sized fractions of recent clastic (riftogenic) sediments and solidified deposits collected from the bottom of the Romanche Trench during the first voyage of R/V Akademik Kurchatov. Similarity between mineral compositions of sediments and bedrocks (ultrabasites, gabbroids, diabases) was established. This similarity is a basis for considering the mineral complex of the deposits that have been derived from the bedrocks of the trench slopes, and have formed due to their submarine denudation accompanied by tectonic crushing. The same mineral composition was found in pieces of older consolidated deposits; this suggests that conditions of sedimentation similar to those at recent times have existed for a long time in the Romanche Trench.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_753708
institution PANGAEA
language en
publishDate 1974
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Chemical composition of ethmodiscus oozes from the Indian Ocean
Sval'nov, Vyacheslav N
Archive of Ocean Data; ARCOD; Calcium carbonate; Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Double leaching by 5% Na2CO3; Elevation of event; Event label; GC; Gravimetric analysis (GF/F filtered); Gravity corer; Indian Ocean; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese oxide; Opal, biogenic silica; PC; Piston corer; Silicon dioxide; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-33; VITYAZ4548; VITYAZ4994; VITYAZ5003; VITYAZ6742-12; VITYAZ6742-18
A study was made of mineral composition of sand- and silt-sized fractions of recent clastic (riftogenic) sediments and solidified deposits collected from the bottom of the Romanche Trench during the first voyage of R/V Akademik Kurchatov. Similarity between mineral compositions of sediments and bedrocks (ultrabasites, gabbroids, diabases) was established. This similarity is a basis for considering the mineral complex of the deposits that have been derived from the bedrocks of the trench slopes, and have formed due to their submarine denudation accompanied by tectonic crushing. The same mineral composition was found in pieces of older consolidated deposits; this suggests that conditions of sedimentation similar to those at recent times have existed for a long time in the Romanche Trench.
title (Table 1) Chemical composition of ethmodiscus oozes from the Indian Ocean
topic Archive of Ocean Data; ARCOD; Calcium carbonate; Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Double leaching by 5% Na2CO3; Elevation of event; Event label; GC; Gravimetric analysis (GF/F filtered); Gravity corer; Indian Ocean; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese oxide; Opal, biogenic silica; PC; Piston corer; Silicon dioxide; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-33; VITYAZ4548; VITYAZ4994; VITYAZ5003; VITYAZ6742-12; VITYAZ6742-18
url https://doi.org/10.1594/PANGAEA.753708