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 |
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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
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Теми: | |
Онлайн доступ: | https://ujrs.org.ua/ujrs/article/view/122 |
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Назва журналу: | Ukrainian Journal of Remote Sensing of the Earth |