Shainurov Turbidity current fan of the Danube submarine canyon
Abstract
Seismic studies at the western part of the deep Black Sea basin proved that the Moiseev Ridge (previously identified on the base of the sea floor topography) did not result from the deep tectonics being a form of turbidity current accumulation, genetically related to the Danube solid discharge.
About the Authors
R. A. Kazantsev
НПО «ЮЖМОРГЕО»
Russian Federation
Russian Federation
R. V. Shainurov
НПО «ЮЖМОРГЕО»
Russian Federation
Russian Federation
Review
For citations:
Kazantsev R.A., Shainurov R.V. Shainurov Turbidity current fan of the Danube submarine canyon. Geomorfologiya. 1978;(3):79-82. (In Russ.)
Views:
90
Email this article 