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Albian-Cenomanian and Santonian-Campanian microfossils as indicators of changing palaeoclimates (Eastern Europe Sector of Russia)тезисы доклада
- Авторы: Kopaevich L.F., Vishnevskaya V.S.
- Сборник: 17th CZECH-SLOVAK-POLISH PALAEONTOLOGICAL CONFERENCE
- Тезисы
- Год издания: 2016
- Место издания: POLISH GEOLOGICAL INSTITUTE- NATIONAL RESEARCH INSTITUTE 4, RAKOWIECKA street, 00-975 WARSAW, POLAND
- Первая страница: 56
- Последняя страница: 56
- Аннотация: The main palaeoceanographic features of the Russian Platform and Crimea-Caucasus area were controlled by the Tethyan/Boreal connection through straits and the influence of sea-level changes. Tectonics during Albian-Cenomanian formed the whole area when rifting took place in the Crimea-Caucasus area. This event resulted in the closing of the Russian Platform longitudinal strait and the opening of a latitudinal sea connection with the European basins and the Tethys region [1]. It is reflected in the foraminiferal and radiolarian zonations for the Upper Cretaceous which are very similar for Western and Central Europe.
- Добавил в систему: Копаевич Людмила Федоровна
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Краткий текст | Kor-Vish-Krakow.docx | 244,9 КБ | 5 ноября 2016 [lfkopaevich] |