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doi: 10.24412/2687-1092-2022-9-128-132 VNIIOkeangeologiya, St. Petersburg, Russia
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Abstract. The Perseus Rise is represented by Mesozoic bedrocks, which are overlain by a very thin cover of Quaternary formations. Using seismoacoustic data, as well as bottom sampling data, the hilly-ridge topography is the result of the impact of Pleistocene glacial and fluvioglacial flows on the bottom. Keywords: geological survey of the shelf, seismoacoustic profiling, bottom sampling, bottom rock material, Perseus Rise, Barents Sea
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Cite this article:
Komarov A.Yu., Gusev E.A., Krylov A.A., Alekseev A.Yu., Semenov P.B., Elkina D.V., Shatrova E.V., Popova E.A., Kartashov A.O., Belyaev P.Yu., Golosnoy A.S., Zakharov V.Yu. 2022. Seafloor of Barents sea on the western slopes of Perseus rise // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 128-132. doi: 10.24412/2687-1092-2022-9-128-132
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