Domes of the Srednepridneprovsky tectonoconcentre of Ukrainian shield
The granite-gneiss domes of the Middle Dnieper were discovered from the data of gravitational and magnetic fields, since Ukrainian shield was significantly denuded and covered by a layer of sedimentary formations of various thicknesses. As a result of the comparison of US geological and geophysical...
Збережено в:
| Дата: | 2018 |
|---|---|
| Автор: | |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
2018
|
| Теми: | |
| Онлайн доступ: | https://ujrs.org.ua/ujrs/article/view/122 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Ukrainian Journal of Remote Sensing of the Earth |
Репозитарії
Ukrainian Journal of Remote Sensing of the Earth| Резюме: | The granite-gneiss domes of the Middle Dnieper were discovered from the data of gravitational and magnetic fields, since Ukrainian shield was significantly denuded and covered by a layer of sedimentary formations of various thicknesses. As a result of the comparison of US geological and geophysical information with the data of the Canadian, Scandinavian and other shields of the planet, a stable assumption about the similarity of their development history arose. It was for understanding the structure of US that the key structural question was not solved - which complexes of natural associations, and why, lie on different denudation sections of it. In numerous described facies, and then in the formations, the questions of the geological development of the shield were not solved. In this work, an attempt is made to clarify some of these issues. |
|---|