Die pleistozäne Vergletscherung im Osten der Russischen Ebene : zentrum im Ural oder Skandinavien?

La glaciation pléistocène dans l'est de la Plaine Russe : une origine en Oural ou en Scandinavie?

Vergletscherungen in europäischen Mittelgebirgen

Glaciations in European Highlands

Auteurs :
DEDKROV, A.P.
BUTAKOV, G.P.
KOSTRZEWSKI, A.

Description :
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.


Type de document :
Congrès

Source :
Colloque international Glaciation of the European Mid-Mountains - in 100th Anniversary of JOSEPH PARTSCH work, Szklarska Poreba, Pologne, 1994, Zeitschrift für Geomorphologie. Supplementband, issn : 0044-2798, 1999, n°. 113, p. 59-67, Collation : Illustration, Références bibliographiques : 11 ref.

Date :
1999

Editeur :
Pays édition : Allemagne, Berlin ; Stuttgart, Borntraeger