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(Article of periodic en Russe - 1989)

Document title


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 l` olaciation de Moscou au Quaternaire, la vallée moyenne de la Protva sert d'exemple (Inconnue)

Authors(s) and Affiliation(s)

ANTONOV S. I. ; BOLYSOV S. I. ; MYSLIVEC V. I. ;

Abstract

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.)

Source

Article of periodic

published at : Geomorfologiâ / ISSN 0435-4281

Editor : Nauka, Moskva - RUSSIE, FEDERATION DE (1970)

Millesime : 1989, no1 [pp. 62-67]

Bibliographic references : 10 réf.

Language

Russe

INIST-CNRS, Cote INIST : 14585

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