Relief formation of the programming shelf of the Taman peninsular
Abstract
The structure and origin of the outer part of Taman peninsular programming shelf are analyzed. This sedimentary prismatic body was formed due to alluvial and deltaic accumulation in periods of the pleistocene transgression.
About the Authors
Yu. A. Pavlidis
Институт океанологии им. П.П. Ширшова РАН
Russian Federation
Russian Federation
F. A. Shcherbakov
Институт океанологии им. П.П. Ширшова РАН
Russian Federation
Russian Federation
Review
For citations:
Pavlidis Yu.A., Shcherbakov F.A. Relief formation of the programming shelf of the Taman peninsular. Geomorfologiya i Paleogeografiya. 1998;(1):91-99.
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