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author Lisitzina, Nadezhda A
Butuzova, Galina Yu
author_facet Lisitzina, Nadezhda A
Butuzova, Galina Yu
collection Datos científicos de ciencias marinas y ambientales
contents Results of petrographic, chemical and X-ray studies of zeolites in sediments in the Transpacific lithological profile from the coast of Japan to the coast of Mexico are reported. For ocean phillipsites constancy of Si/Al ratio (2.44-2.87) and unstable cation composition in quantitative predominance of potassium over sodium are characteristic. Two groups of ocean phillipsites are distinguished: of deep-water basins and of submarine rises. The first spread over broad areas of the pelagic zone, and are formed by diagenetic transformation of fine dispersed pyroclastic material in minimum sedimentation rates, the latter occur locally - in areas of basaltic volcanism manifestations.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_777549
institution PANGAEA
language en
publishDate 1976
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Chemical composition of phillipsites from pelagic bottom sediments of the Transpacific profile
Lisitzina, Nadezhda A
Butuzova, Galina Yu
Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Barium oxide; Calcium oxide; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-612; DM9-643; Dmitry Mendeleev; Elevation of event; Event label; GC; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Northeast Pacific; Northwestern Basin, Pacific Ocean; Northwest Pacific; OKEAN; Okean Grab; Phosphorus pentoxide; Potassium oxide; Ratio; Silicon/Aluminium ratio; Silicon dioxide; Size fraction; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ4362-GR-1; VITYAZ6176-GC; VITYAZ6177-GR; Water in rock; Wet chemistry
Results of petrographic, chemical and X-ray studies of zeolites in sediments in the Transpacific lithological profile from the coast of Japan to the coast of Mexico are reported. For ocean phillipsites constancy of Si/Al ratio (2.44-2.87) and unstable cation composition in quantitative predominance of potassium over sodium are characteristic. Two groups of ocean phillipsites are distinguished: of deep-water basins and of submarine rises. The first spread over broad areas of the pelagic zone, and are formed by diagenetic transformation of fine dispersed pyroclastic material in minimum sedimentation rates, the latter occur locally - in areas of basaltic volcanism manifestations.
title (Table 1) Chemical composition of phillipsites from pelagic bottom sediments of the Transpacific profile
topic Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Barium oxide; Calcium oxide; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-612; DM9-643; Dmitry Mendeleev; Elevation of event; Event label; GC; Gravity corer; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Northeast Pacific; Northwestern Basin, Pacific Ocean; Northwest Pacific; OKEAN; Okean Grab; Phosphorus pentoxide; Potassium oxide; Ratio; Silicon/Aluminium ratio; Silicon dioxide; Size fraction; Sodium oxide; Sum; Titanium dioxide; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ4362-GR-1; VITYAZ6176-GC; VITYAZ6177-GR; Water in rock; Wet chemistry
url https://doi.org/10.1594/PANGAEA.777549