IGB

Connexion

(Szklarska PorebaColloque international Glaciation of the European Mid-Mountains - in 100th Anniversary of JOSEPH PARTSCH work en Allemand - 1999)

Document title

Die pleistozäne Vergletscherung im Osten der Russischen Ebene : zentrum im Ural oder Skandinavien? (Allemand)
La glaciation pléistocène dans l'est de la Plaine Russe : une origine en Oural ou en Scandinavie?

published at : Vergletscherungen in europäischen Mittelgebirgen
Glaciations in European Highlands (Anglais)

Authors(s) and Affiliation(s)

DEDKROV A.P. ; BUTAKOV G.P. ;

Abstract

The discussion about correlation of the Ural and Scandinavian glaciations lasted about 100 years. In the course of longterm investigations it has been established that the desintegrated rocks scattered on the surface are derived of Permian and Mesozoic conglomerates (petrographic and granulometric composition, roudness and other features). 2 complexes can be identified in this material. The difference in their composition displays the difference in climatic conditions during the denudation of the Ural. The north and west of the Ural were covered only by the Scandinavian glacier

Source

Congrès

Colloque international Glaciation of the European Mid-Mountains - in 100th Anniversary of JOSEPH PARTSCH work, Szklarska Poreba , POLOGNE ()

published at : Zeitschrift für Geomorphologie. Supplementband / ISSN 0044-2798

Editor : Borntraeger, Berlin ; Borntraeger, Stuttgart - ALLEMAGNE (1960)

Millesime : 1999, no 113 [pp. 59-67]

Bibliographic references : 11 ref.

Language

Allemand

Localisation

Laboratoire INTERGEO - Paris

INIST-CNRS, Cote INIST : 8829 B

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1999.
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