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author Baturin, Gleb N
Korytov, F Ya
author_facet Baturin, Gleb N
Korytov, F Ya
collection Datos científicos de ciencias marinas y ambientales
contents Fluorine concentrations were determined ionometrically with an error of 0.02% in iron-manganese materials of the ocean. They were: 0.02-0.04% in ocean iron-manganese nodules, with the exception of two specimens (0.08% and 0.20% F); up to 0.02% in iron-manganese nodules of seas; 0.02-1.17% in ore crusts from ocean seamounts; and 0.02% in ore sediments of the Red Sea. Elevated fluorine content of ore crusts is associated with presence of calcium phosphate inclusions in them. Fluorine is not accumulated during iron-manganese nodule mineralization. Its average concentration in the nodules is half that in host deep-sea sediments.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_757446
institution PANGAEA
language en
publishDate 1988
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of Fe-Mn nodules and crusts from oceans and seas
Baturin, Gleb N
Korytov, F Ya
Archive of Ocean Data; ARCOD; Area/locality; Atlantic Ocean; Atomic absorption spectrometry (AAS); BK-1664; BK-26A; BK-2754; BK-2842; BK-2852; BK-2875; BK-2876; BK-4216; BK-4224; BK-666-1; Black Sea; Calculated; Central Pacific Seamounts, Pacific Ocean; DM35-3136; Dredge; DRG; Elevation of event; Event label; Fluorine; Indian Ocean; Iron; Latitude of event; Longitude of event; Manganese; Manganese/Iron ratio; MULT; Multiple investigations; Pacific Ocean; Phosphorus; Sample type; Unnamed seamount; VITYAZ; Vityaz (ex-Mars); Vityaz-2; Vityaz-2-8; Vityaz-35; Vityaz-43; Vityaz-48; VITYAZ5193; VITYAZ5201; VITYAZ6002; VITYAZ6348; VITYAZ6359; VITYAZ6366; Vy-798; Wet chemistry
Fluorine concentrations were determined ionometrically with an error of 0.02% in iron-manganese materials of the ocean. They were: 0.02-0.04% in ocean iron-manganese nodules, with the exception of two specimens (0.08% and 0.20% F); up to 0.02% in iron-manganese nodules of seas; 0.02-1.17% in ore crusts from ocean seamounts; and 0.02% in ore sediments of the Red Sea. Elevated fluorine content of ore crusts is associated with presence of calcium phosphate inclusions in them. Fluorine is not accumulated during iron-manganese nodule mineralization. Its average concentration in the nodules is half that in host deep-sea sediments.
title Chemical composition of Fe-Mn nodules and crusts from oceans and seas
topic Archive of Ocean Data; ARCOD; Area/locality; Atlantic Ocean; Atomic absorption spectrometry (AAS); BK-1664; BK-26A; BK-2754; BK-2842; BK-2852; BK-2875; BK-2876; BK-4216; BK-4224; BK-666-1; Black Sea; Calculated; Central Pacific Seamounts, Pacific Ocean; DM35-3136; Dredge; DRG; Elevation of event; Event label; Fluorine; Indian Ocean; Iron; Latitude of event; Longitude of event; Manganese; Manganese/Iron ratio; MULT; Multiple investigations; Pacific Ocean; Phosphorus; Sample type; Unnamed seamount; VITYAZ; Vityaz (ex-Mars); Vityaz-2; Vityaz-2-8; Vityaz-35; Vityaz-43; Vityaz-48; VITYAZ5193; VITYAZ5201; VITYAZ6002; VITYAZ6348; VITYAZ6359; VITYAZ6366; Vy-798; Wet chemistry
url https://doi.org/10.1594/PANGAEA.757446