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author Krämer, Tom
Schornick, James C
author_facet Krämer, Tom
Schornick, James C
collection Datos científicos de ciencias marinas y ambientales
contents The chemical composition of layered deposit inside zones has been determined for ferromanganese nodules and crusts retrieved in the South Pacific Ocean during various R/V Eltanin cruises. Samples were prepared from the nodules and crusts by peeling or scraping successive layers and measuring the resultant decrease in thickness with calipers. The samples were then ground to a fine powder and split into two aliquots, one for U and Th isotopic analysis, the other for elemental analysis. Mercury was determined by flameless atomic absorption spectrophotometry. The remaining elements were determined by standard atomic absorption spectrophotometry. The errors for all elemental determinations are estimated to be 10% or better.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_954698
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of the internal layers of manganese deposits from the South Pacific Ocean
Krämer, Tom
Schornick, James C
Atomic absorption spectrophotometry; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Distance; Distance, maximum; Distance, minimum; Dredge, rock; DRG_R; Elevation of event; ELT05; ELT05.004SS-RD; ELT15; ELT15.013-PC; ELT21; ELT21.004-BT; ELT24; ELT24.015-RS; Eltanin; Event label; Flameless atomic absorption spectrophotometry; Geochemistry; Identification; Iron; Latitude of event; Lead; Longitude of event; Manganese; manganese micronodule; manganese nodule; Mercury; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; PC; Piston corer; Sediment; Southern Ocean; South Pacific Ocean; Thorium; TRAWL; Trawl net; Uranium; Zinc
The chemical composition of layered deposit inside zones has been determined for ferromanganese nodules and crusts retrieved in the South Pacific Ocean during various R/V Eltanin cruises. Samples were prepared from the nodules and crusts by peeling or scraping successive layers and measuring the resultant decrease in thickness with calipers. The samples were then ground to a fine powder and split into two aliquots, one for U and Th isotopic analysis, the other for elemental analysis. Mercury was determined by flameless atomic absorption spectrophotometry. The remaining elements were determined by standard atomic absorption spectrophotometry. The errors for all elemental determinations are estimated to be 10% or better.
title Chemical composition of the internal layers of manganese deposits from the South Pacific Ocean
topic Atomic absorption spectrophotometry; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Distance; Distance, maximum; Distance, minimum; Dredge, rock; DRG_R; Elevation of event; ELT05; ELT05.004SS-RD; ELT15; ELT15.013-PC; ELT21; ELT21.004-BT; ELT24; ELT24.015-RS; Eltanin; Event label; Flameless atomic absorption spectrophotometry; Geochemistry; Identification; Iron; Latitude of event; Lead; Longitude of event; Manganese; manganese micronodule; manganese nodule; Mercury; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; PC; Piston corer; Sediment; Southern Ocean; South Pacific Ocean; Thorium; TRAWL; Trawl net; Uranium; Zinc
url https://doi.org/10.1594/PANGAEA.954698