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(Article of periodic en Anglais - 1995)

Document title

The margin of the last Barents-Kara ice sheet at Markhida, northern Russia

Authors(s) and Affiliation(s)

TVERANGER J. ; ASTAKHOV V. ; MANGERUD J. ;

Abstract

The crucial point in the glaciation history proposed by Grosswald and Arslanov is the genesis of the upper diamicton at Markhida, interpreted as a basal till deposited under a dynamic, active glacier after about 9500 C-14 yr B.P. The primary aim of this reexamination of the section, therefore, was to establish the age and clarify the genesis of the Markhida Moraine at its type site in order to test the existing models of glaciation in the area

Source

Article of periodic

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

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

Millesime : 1995, vol. 44, no3 [pp. 328-340]

Bibliographic references : 25 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1996.
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