Zobrazeno 1 - 10
of 16
pro vyhledávání: '"K. V. Syromyatnikov"'
Autor:
R. R. Gabdullin, A. Yu. Puzik, S. I. Merenkova, E. A. Bakay, E. N. Poludetkina, K. V. Syromyatnikov, M. D. Kazurov, I. R. Migranov, S. I. Bordunov, M. A. Ustinova, Yu. I. Rostovtseva, D. A. Маmontov, N. V. Badulina, A. V. Ivanov
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :46-55
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::829414fc59075cc83085b4385819ec90
https://doi.org/10.33623/0579-9406-2022-6-46-55
https://doi.org/10.33623/0579-9406-2022-6-46-55
Autor:
K. V. Syromyatnikov, R. R. Gabdullin
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :51-61
In this article, the possibilities of statistical analysis methods were demonstrated on the example of studying modern bottom sediments in the western part of the Barents Sea. As a result of cluster and dispersion analyses, regularities in the distri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ff6bc5e91eed41110b8edf8e6490a29
https://doi.org/10.33623/0579-9406-2022-4-51-61
https://doi.org/10.33623/0579-9406-2022-4-51-61
Autor:
K. V. Syromyatnikov, R. R. Gabdullin
Publikováno v:
Moscow University Geology Bulletin. 77:714-728
In the article, methods of mathematical statistics were used to study the processes of sedimentogenesis and early diagenesis of the surface sediments of the Kara Sea. Correlation analysis established two groups of oxides associated with certain granu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::430d049ba6ea77777a0866fee465598f
https://doi.org/10.3103/s0145875222060126
https://doi.org/10.3103/s0145875222060126
Autor:
K. V. Syromyatnikov, R. R. Gabdullin
Publikováno v:
Moscow University Geology Bulletin. 77:497-507
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6676c8aa7ac33425d0514a31a5ac5dac
https://doi.org/10.3103/s0145875222050155
https://doi.org/10.3103/s0145875222050155
Autor:
M. A. Levitan, T. A. Antonova, T. N. Gelvi, L. G. Domoratskaya, A. V. Koltsova, K. V. Syromyatnikov
Publikováno v:
Geochemistry International. 60:551-559
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4267ebd953d2fc645b75d7382d3344d2
https://doi.org/10.1134/s0016702922050068
https://doi.org/10.1134/s0016702922050068
Publikováno v:
Geochemistry International. 59:577-584
The lithological-facies zoning of the Neo- and Eopleistocene sediments of submarine continental margin of Southwestern Africa was described for the first time using deep-sea drilling data. Corresponding maps with isopachs were processed using A.B. Ro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ec374545cc17402ff3d18959582c49b
https://doi.org/10.1134/s0016702921060069
https://doi.org/10.1134/s0016702921060069
Publikováno v:
Geochemistry International. 59:413-421
The lithological-facies zoning of the Neo- and Eopleistocene sediments of the Caribbean Sea has been described for the first time based on deep-sea drilling data. Сorresponding maps and isopach schemes were processed using A.B. Ronov’s volumetric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e234172a4c95f84688a60e3dadcbd60b
https://doi.org/10.1134/s0016702921040030
https://doi.org/10.1134/s0016702921040030
Autor:
K. V. Syromyatnikov, Mikhail A Levitan
Publikováno v:
Geochemistry International. 59:127-138
The variance and regression analyses were applied to study the distribution and relationships between organic carbon, calcium carbonate, abiogenic matter, biogenic silica, and their accumulation depth in the upper Pliocene sediments in different stru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::73b5112e5d8631930815037e1f9b2841
https://doi.org/10.1134/s0016702921020075
https://doi.org/10.1134/s0016702921020075
Publikováno v:
Geochemistry International. 56:304-317
Lithofacies zoning is described for the first time for the Neo- and Eopleistocene of the Bering Sea. Four lithofacies sedimentation zones are distinguished: (I) terrigenous; (II) siliceous–terrigenous; (III) siliceous, and (IV) volcanoterrigenous o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9daa4464a0db4045c7675ea2792419e
https://doi.org/10.1134/s0016702918040055
https://doi.org/10.1134/s0016702918040055
Publikováno v:
Geochemistry International. 55:503-520
Holocene sequences of the Russian Arctic shelf seas are controlled by a combination of three main factors: deglaciation of the Late Pleistocene Barents–Kara ice sheet, global sea-level rise, and river runoff from Eurasia. Sedimentation in the Kara
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d349195e3622ff21a4e807decb6c054
https://doi.org/10.1134/s001670291706009x
https://doi.org/10.1134/s001670291706009x