STRATIGRAPHY OF LOWER CENOMANIANS FORMATIONS OF NORTH-WEST PRICHERNOMOR'E, MIDDLE PRIDNIESTROV'E AND EAST REGION OF VOLYNO- PODOL'E
Complex analysis of paleontological remains, lithology and cyclic recurrence of sedimentation Lower Cenomanians formations of considered regions have been allowed to obtain for first time the sediments of three basins (Black Sea coast, Carpatian, Borealen (Buelorussian)) and correlate their relation...
Збережено в:
Дата: | 2010 |
---|---|
Автори: | , , , |
Формат: | Стаття |
Мова: | rus |
Опубліковано: |
Institute of Geological Sciences, NAS of Ukraine
2010
|
Теми: | |
Онлайн доступ: | http://geojournal.igs-nas.org.ua/article/view/220687 |
Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
Назва журналу: | Geological journal |
Репозитарії
Geological journalРезюме: | Complex analysis of paleontological remains, lithology and cyclic recurrence of sedimentation Lower Cenomanians formations of considered regions have been allowed to obtain for first time the sediments of three basins (Black Sea coast, Carpatian, Borealen (Buelorussian)) and correlate their relationships. For first time two suites for the formations of the Black Sea coast basin have been established: early – Glubochekska, that correlated with Carpatian basin sediments – sandy-gaize rock masses and its analoges in the Middle Near-Dniester, Moldava, Volyn (bottom bench); upper – Trostjanetska, that correlated with rocks of Barealen (Buelorussian) sea an Volyn (top bench), named as Stublatska there. |
---|