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doi: 10.24412/2687-1092-2022-9-285-290 1 Lomonosov Moscow State University, Moscow, Russia 2 Institute of Geography, Russian Academy of Sciences, Moscow, Russia 3 DecoGeophysics, Moscow, Russia 4 St. Petersburg State University, St. Petersburg, Russia 5 RN-Exploration, Moscow, Russia
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Abstract. The problem of the Barents Sea Ice Sheet southern boundary location is one of the controversial issues of the paleogeography of the region. The paper summarizes the published data on the distribution of erosion-accumulation geological formations characteristic of glacial and periglacial shelves on the Pechora shelf. Based on the interpretation of standard seismic exploration data 2D and 3D reconstructed a network of paleochannels that can be compared with the Pra Pechora valley. The boundaries of the distribution of perennial breeds have been clarified. The evidence is given that during the last glacial maximum the glaciation boundary was in the area of the «Kolguyev line», and on the coastal shallow water there were periglacial conditions. Keywords: Pechora Sea, relief, Valdai glaciation, permafrost rock mass, river Pra-Pechora
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Cite this article:
Khlebnikova O.A., Repkina T.Y., Terekhina J.E., Solovyeva M.A., Rybalko A.E., Kolubakin A.A. 2022. New data on signs of the maximum extent of the last glaciation in the Pechora Sea // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 285-290. doi: 10.24412/2687-1092-2022-9-285-290
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