Razvitie dolin malyh rek v central'noj casti kraevoj zony Moskovskogo oledenenija v cetverticnoe vremja (na primere srednej Protvy) Evolution des vallées de petites rivières dans la partie centrale de la zone marginale de la glaciation de Moscou au Quaternaire, la vallée moyenne de la Protva sert d'exemple

Auteurs :
ANTONOV, S. I.
BOLYSOV, S. I.
MYSLIVEC, V. I.

Description :
Field studies in the Protva drainage basin elucidated the drainage network evolution. Some small valleys and erosional landforms date back to Pre-Quaternary time. Erosion and alluviation states alternated throughout the Pleistocene, erosion took place early during interglacial or warm phases, alluviation proceeded mostly during early glacial, full glacial and late glacial time. Erosion-alluviation alternation was mostly controlled by climate and in lesser degree by isostasy and neotectonics. Most of the valleys were inherited from Pre-Quaternary froms and developed continuously. - (L'A.).


Type de document :
Article de périodique

Source :
Geomorfologiâ (Moskva), issn : 0435-4281, 1989, n°. 1, p. 62-67, Références bibliographiques : 10 réf.

Date :
1989

Editeur :
Pays édition : Russie, Federation de, Moskva, Nauka