Mineralogical Characteristics of the Sand Fraction in Quaternary Sediments from the Southern Margin of the Chukchi Plateau, Arctic Ocean
- Autores: Kolesnik O.N.1, Kolesnik A.N.1, Vologina E.G.2, Maryash A.A.1
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Afiliações:
- Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences
- Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences
- Edição: Volume 59, Nº 4 (2019)
- Páginas: 556-576
- Seção: Marine Geology
- URL: https://journals.rcsi.science/0001-4370/article/view/149906
- DOI: https://doi.org/10.1134/S000143701904009X
- ID: 149906
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Resumo
The paper presents mineralogical analysis data on very-fine- and fine-grained sand in the composition of Quaternary sediments in the southern part of the Chukchi Plateau. The associations and downcore distribution of rock-forming and accessory minerals in relation to other characteristics are considered. The established climatically controlled mineralogical features, i.e., periodicity of warmings and coolings, can be used to solve a number of genetic problems, stratigraphic subdivision of sediments, and paleoreconstructions.
Sobre autores
O. Kolesnik
Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences
Autor responsável pela correspondência
Email: kolesnik_o@poi.dvo.ru
Rússia, Vladivostok, 690041
A. Kolesnik
Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences
Email: kolesnik_o@poi.dvo.ru
Rússia, Vladivostok, 690041
E. Vologina
Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences
Email: kolesnik_o@poi.dvo.ru
Rússia, Irkutsk, 664033
A. Maryash
Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences
Email: kolesnik_o@poi.dvo.ru
Rússia, Vladivostok, 690041
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