Chemical composition of ferromanganese concretions and host bottom sediments from the Black Sea

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Main Author: Baturin, Gleb N
Format: Dataset Open Access
Language:en
Published: PANGAEA 2010
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author Baturin, Gleb N
author_facet Baturin, Gleb N
collection Datos científicos de ciencias marinas y ambientales
contents Ferromanganese concretions spread out on the bottom of the shallow northwest part of the Black Sea are mainly represented by Fe and Mn nodules on shells and substituted worm tubes. Element composition of these formations was measured by methods of chemical, atomic absorbtion, neutron activation, and ICP-MS analyses. It was established that Fe and Mn contents and Mn/Fe ratio in the concretions varied considerably and which controlled occurrence of several associated metals and minor elements; some of them have not been studied in Black Sea concretions before.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_763679
institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of ferromanganese concretions and host bottom sediments from the Black Sea
Baturin, Gleb N
Archive of Ocean Data; ARCOD; Black Sea; GC; Gravity corer; OKEAN; Okean Grab; Vityaz-2; Vityaz-2-8; Vy-798-2; Vy-800-3; Vy-802; Vy-848-1; Vy-891
Ferromanganese concretions spread out on the bottom of the shallow northwest part of the Black Sea are mainly represented by Fe and Mn nodules on shells and substituted worm tubes. Element composition of these formations was measured by methods of chemical, atomic absorbtion, neutron activation, and ICP-MS analyses. It was established that Fe and Mn contents and Mn/Fe ratio in the concretions varied considerably and which controlled occurrence of several associated metals and minor elements; some of them have not been studied in Black Sea concretions before.
title Chemical composition of ferromanganese concretions and host bottom sediments from the Black Sea
topic Archive of Ocean Data; ARCOD; Black Sea; GC; Gravity corer; OKEAN; Okean Grab; Vityaz-2; Vityaz-2-8; Vy-798-2; Vy-800-3; Vy-802; Vy-848-1; Vy-891
url https://doi.org/10.1594/PANGAEA.763679