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doi: 10.24412/2687-1092-2023-10-261-268
1Lomonosov Moscow State University, Moscow, Russia 2Saint Petersburg State University, Saint Petersburg, Russia 3Scott Polar Research Institute, University of Cambridge, Cambridge, UK 4LLC «RN-Exploration», Moscow, Russia
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Abstract. The study demonstrates an analysis of the most representative database of 2D/3D seismic survey, engineering-geophysical survey, multibeam echosounding and bottom sampling in the Russian sector of the Barents Sea. As the result, a wide variety of glacial landforms were detected and mapped. Peculiarities of their distribution suggest that the ice-sheet glaciation was developed on the entire Barents Sea shelf. Analysis of glacial landforms allowed reconstructing the evolution of the glaciation in the Late Weichselian, making the pre-existing models significantly better detailed. Directions of ice streams as well as positions of marine-based ice dome were revealed. Keywords: Barents Sea, multibeam echosounding, 2D/3D seismic, glacial landforms, Weichselian glaciation, paleogeographic reconstructions
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Cite this article:
Solovyeva M.A., Rybalko A.E., Montelli A.I., Terekhina Ya.E., Kolubakin A.A., Tokarev M.Yu., Akhmanov G.G. The Weichselian glaciation in the Eastern Barents Sea // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2023. Issue 10. P. 261-268. doi: 10.24412/2687-1092-2023-10-261-268
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