Отправить статью по E-mail Facies Structure and Quantitative Parameters of Pleistocene Sediments from the East Australian Continental Margin
- Авторы: Levitan M.A.1, Antonova T.A.1, Koltsova A.V.1
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Учреждения:
- Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
- Выпуск: Том 57, № 6 (2019)
- Страницы: 698-708
- Раздел: Article
- URL: https://journals.rcsi.science/0016-7029/article/view/156209
- DOI: https://doi.org/10.1134/S0016702919060053
- ID: 156209
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Аннотация
Abstract—Lithological and facies zonality of Neopleistocene and Eopleistocene sediments of the Australian seas is described for the first time. Processing of these maps and isopach schemes by A.B. Ronov volumetric method gave us an opportunity to calculate the quantitative parameters of sedimentation for different types of the Pleistocene sediments. It was revealed that carbonate sediments predominate over other sediment groups. The Neopleistocene was characterized by more intense accumulation of carbonate planktic sediments and lithogenic sediments than Eopleistocene.
Об авторах
M. Levitan
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: m-levitan@mail.ru
Россия, ul. Kosygina, 19, Moscow, 119991
T. Antonova
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Email: m-levitan@mail.ru
Россия, ul. Kosygina, 19, Moscow, 119991
A. Koltsova
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Email: m-levitan@mail.ru
Россия, ul. Kosygina, 19, Moscow, 119991
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