Аннотация
Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events.
Язык оригинала | английский |
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Страницы (с-по) | 72-87 |
Число страниц | 16 |
Журнал | Russian Geology and Geophysics |
Том | 59 |
Номер выпуска | 1 |
DOI | |
Состояние | Опубликовано - 1 янв 2018 |