Zobrazeno 1 - 8
of 8
pro vyhledávání: '"S. L. Nikiforov"'
Autor:
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
Publikováno v:
Oceanology. 62:540-549
Abstract The article deals with the issues of the geodynamic evolution of the Kara–Barents Sea shelf and influence of structure-forming processes on the nature of relief formation. The aggregate data obtained allows us to assume that the relief of
Autor:
I. V. Chickiryov, D. S. Tolstobrov, N. O. Sorokhtin, S. L. Nikiforov, A. A. Melousov, R. A. Ananiev, N. N. Dmitrevsky
Publikováno v:
Vestnik MGTU, Vol 24, Iss 1, Pp 131-141 (2021)
In August - September 2020, during cruise 49 of the R/V Akademik Nikolay Strakhov , comprehensive geological, geophysical, hydroacoustic, geomorphological and hydrophysical research studies of the western segment of the Arctic zone within the Pechora
Publikováno v:
Oceanology. 62:433-434
Autor:
S. L. Nikiforov, N. O. Sorokhtin, N. N. Dmitrevskiy, R. A. Ananiev, S. Y. Sokolov, A. K. Ambrosimov, A. А. Meluzov, A. D. Mutovkin
Publikováno v:
Океанология. 59:885-887
The first results of the multidisciplinary expedition onboard research vessel Akademik Nikolaj Strakhov in the Barents Sea in August-September 2018 are given. On 41 stations the hydrophysical sounding was carried out, sampling of the bottom sediments
Autor:
N. O. Sorokhtin, O. Yu. Bogdanova, G. V. Novikov, L. I. Lobkovsky, E. E. Kozlov, S. L. Nikiforov
Publikováno v:
Oceanology. 56:572-577
This paper discusses the geodynamic evolution of the lithosphere in the Arctic region during the Phaneorozic and its polyphase lithotectonic reorganization. Spatiotemporal patterns of the mosaic junction of lithospheric plates of different age are pr
Publikováno v:
Океанология. 55:326-336
Autor:
S. L. Nikiforov
Publikováno v:
Polar Geography and Geology. 14:287-293
A marine regression synchronous with and associated with the late‐Pleistocene Sartan Glaciation exposed large areas of the shelf in the Chukchi and East Siberian seas; areas of the sea bed now lying at depths of up to 50–55 m were exposed. The ar