ПЕРСПЕКТИВИ ГАЗОНОСНОСТІ ОБЛАСТІ ЗЧЛЕНУВАННЯ ДНІПРОВСЬКОГО ГРАБЕНА ТА ДОНЕЦЬКОЇ СКЛАДЧАСТОЇ СПОРУДИ
The location of Karlivka depression is described in this article. The depression is considered as a special geodynamic joint area of the Dnipro graben and Donetsk folded structure. The Phanerozoic geodynamic scale is used together with structural-facial complexes (SFC) developed by V.K. Gavrysh for...
Збережено в:
| Дата: | 2019 |
|---|---|
| Автор: | |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Institute of Geological Sciences of the Ukrainian National Academy of Sciences
2019
|
| Теми: | |
| Онлайн доступ: | http://ts.igs-nas.org.ua/article/view/208877 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Tectonics and stratigraphy |
Репозитарії
Tectonics and stratigraphy| Резюме: | The location of Karlivka depression is described in this article. The depression is considered as a special geodynamic joint area of the Dnipro graben and Donetsk folded structure. The Phanerozoic geodynamic scale is used together with structural-facial complexes (SFC) developed by V.K. Gavrysh for the Dnieper-Donets Rift. The geodynamic joint area has a crescent shape and is the center of anomalous Early Permian deposits first described by I.I. Demianenko. The Permian Earth’s crust development is the beginning of the Alpine stage of the Earth’s expansion, which rocks (the Early Permian) are characterized by remarkable storage capacity, as well as the further Late Triassic and Early Cretaceous beddings. The integrated processing of remote sensing data and seismic measurements allowed to divide into districts the regional seismic profile named Lozova-Shebelynka-Staropokrivka in accordance with gas potential. |
|---|