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Sorokhtin N. O., Nikiforov S. L., Koshel S. M., Kozlov N. E.
Geodynamic evolution and orphostructural analysis of the Western sector of the Russian Arctic shelf
DOI: 10.21443/1560-9278-2016-1/1-123-137
- Rare and Trace Elements in the Modern Bottom Sediments of the Barents Sea
A. V. Maslov, N. V. Politova, N. V. Kozina, V. P. Shevchenko, T. N. Alekseeva
Lithology and Mineral Resources, 2020; 55(1): 1 - Impact of seasonal variations of ambient seismic noise level on the number of registered earthquakes in the Arctic regions
ER Morozova, AP Turova
Arctic Environmental Research, 2019; 19(3): 123 - Geodynamics of the Russian Arctic Shelf and Relief-Forming Processes in the Central Kara Basin
N. O. Sorokhtin, S. L. Nikiforov, R. A. Ananiev, N. N. Dmitrevskiy, E. A. Moroz, E. A. Sukhih, N. E. Kozlov, I. V. Chikirev, A. I. Fridenberg, A. A. Koluibakin
Oceanology, 2022; 62(4): 540 - Co, Hf, Ce, Cr, Th, and REE Charateristics of Modern Bottom Sediments of the Barents Sea
A. V. Maslov, N. V. Politova, V. P. Shevchenko, N. V. Kozina, A. N. Novigatsky, M. D. Kravchishina
Doklady Earth Sciences, 2019; 485(1): 298 - Distribution of Trace and Rare-Earth Elements, and Nd, Pb, and Sr Isotopes in the Surface Sediments of the Barents Sea
A. V. Maslov, A. B. Kuznetsov, N. V. Politova, V. P. Shevchenko, N. V. Kozina, A. N. Novigatsky, M. D. Kravchishina, T. N. Alexeeva
Geochemistry International, 2020; 58(6): 687
Abstract. The paper considers issues of the Barents Sea shelf geodynamic evolution and influence of basement geologic structural processes on seabed morphology in their interaction. The obtained data have made possible to assume that the Norwegian-Mezenskaya rift system, Voronin graben, St. Anne and Victoria grabens were formed at the expense of the lithosphere stretching processes, but the Vostochno-Barentsevomorskaya basin and Medvezinsko-Edzinskaya area of depressions developed on the initial stage of lithosphere plate evolution due to collision of several island arcs and now all of them are outliers of the ancient oceanic crust. The technique of morphostructural analysis developed by the authors has allowed solve the inverse problem, and under morphological approach split all largest depressions on two main genetic types that confirm received geodynamic conclusion
Keywords: geodynamics, morphostructural analysis, the Barents Sea shelf, seabed morphology
Printed reference: Geodynamic evolution and orphostructural analysis of the Western sector of the Russian Arctic shelf / N. Sorokhtin, S. Nikiforov, S. Koshel, N. Kozlov // Vestnik of MSTU. 2016. V. 19, No 1. P. 123-137.
Electronic reference: Geodynamic evolution and orphostructural analysis of the Western sector of the Russian Arctic shelf / N. Sorokhtin, S. Nikiforov, S. Koshel, N. Kozlov // Vestnik of MSTU. 2016. V. 19, No 1. P. 123-137. URL: http://vestnik.mstu.edu.ru/v19_1_1n64/15_Sorokhtin_123_137.pdf.
