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(Article of periodic en Anglais - 1992)

Document title

Evidence for the dissolution of magnetite in recent Scottish peats

Authors(s) and Affiliation(s)

WILLIAMS M. ;

Abstract

Magnetic, hydrological, and geochemical data for 11 Scottish peat cores confirm previous reports that anthropogenic pollutants constitute the principal source of ferrimagnets to such environments, but indicate that postdepositional Fe[3]O[4] persistence may be more limited than formerly envisaged. Rates of dissolution are considerably greater than those reported for marine sediments, probably due to the unusually high dissolved sulfide concentrations in mire waters

Source

Article of periodic

published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV

Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)

Millesime : 1992, vol. 37, no2 [pp. 171-182]

Bibliographic references : 38 réf.

Collation : Illustration ;

Language

Anglais

Localisation

American geological institute

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1993.
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