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The Devonian and Carboniferous of the Moscow Syneclise (Russian Platform): Stratigraphy and sea-level changesстатья
Информация о цитировании статьи получена из
Scopus,
Web of Science
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.
- Авторы: Alekseev A.S., Kononova L.I., Nikishin A.M.
- Журнал: Tectonophysics
- Том: 268
- Номер: 1-4
- Год издания: 1996
- Издательство: Elsevier BV
- Местоположение издательства: Netherlands
- Первая страница: 149
- Последняя страница: 168
- Аннотация: The Moscow Syneclise is a vast sedimentary basin located in the centre of the East-European Platform. The Palaeozoic sequence of this syneclise, and especially its Devonian-Carboniferous part, is most suitable for sea-level fluctuation analysis. The Devonian and Carboniferous sediments consist mainly of shallow-marine carbonates, containing several minor terrigenous intervals; they attain total thicknesses of up to 1.5 km. The modern stratigraphic scale includes 33 regional stages for the Devonian and 32 for the Carboniferous. Correlation of this scale with global scales is supported by conodont, miospore and foraminifera zonations. The new calibrated Devonian and Carboniferous relative sea-level curves for the Moscow Syneclise reflect late Eifelian, mid-Frasnian, early Tournaisian, late Visean-early Serpukhovian and Moscovian-Gzhelian transgressions. Several of these sea-level changes, which are particularly evident on the margins of the Moscow Syneclise, originated in response to differential tectonic movements of the Voronezh Anteclise and the Tokmovo Uplift as well as to vertical oscillations of the entire East-European craton.
- Добавил в систему: Никишин Анатолий Михайлович