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(Article of periodic en Russe - 1988)

Document title


O stroenii glubokovodnogo Dunajskogo konusa vynosa Structure du cône sous-marin du Danube (Inconnue)

Authors(s) and Affiliation(s)

KULAKOVA L. S. ; LEBEDEV L. I. ;

Abstract

On the basis of geoacoustic profiling data three generations have been distinguished within the deep-sea fan of the Danube River (older than Middle Pleistocene, Middle Pleistocene, Late Pleistocene - Holocene ones). Schematic maps of the sediments thickness are compiled for the two younger generations. The principal fan structure includes accessory lenses of sediments, formed by the material sliding along the fan's slopes. The position of the axial trough and levees of the present-day Danube fan appeared to be inconsistent with those of older fans due to migration of the Danube's mouth. - (Ed.)

Source

Article of periodic

published at : Geomorfologiâ / ISSN 0435-4281

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

Millesime : 1988, no2 [pp. 79-85]

Bibliographic references : 9 réf.

Language

Russe

INIST-CNRS, Cote INIST : 14585

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