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doi: 10.24412/2687-1092-2024-11-444-449
1 VNIIOkeangeologia, St. Petersburg, Russia 2 Saint-Petersburg State University, St. Petersburg, Russia 3 Arctic and Antarctic Research Institute, St. Petersburg, Russia
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Abstract. The paper presents the paleomagnetic results on a sediment core of more than 4-m length, recovered by a gravity corer in the Amundsen Basin, during the Severnyi Polyus 41 expedition. These studies are one of the few paleomagnetic studies in the Eurasian Basin and practically one of the only in the Amundsen Basin. High positive inclinations together with several short intervals of well-defined negative inclinations of the calculated characteristic magnetization component, supported by low maximum angular deviation, can be further used to construct magnetostratigraphy and calculate average sedimentation rates in the area. Keywords: sediment cores, Arctic Ocean, Amundsen Basin, paleomagnetic studies, Eurasian Basin
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Cite this article:
Elkina D.V., Piskarev A.L., Khosnullina T.I., Gusev E.A., Popova E.A., Bogin V.A., Malyshev S.A., Filchuk K.V., Makarov A.S. First paleomagnetic results on marine sediments collected in the Amundsen basin, Arctic ocean. Results of expedition North Pole-41 // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2024. Issue 11. P. 444-449. doi: 10.24412/2687-1092-2024-11-444-449
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