Pripyat trough as a possible channel of mantle degassing: deep structure and position in the junction zone of Sarmatia and Fennoscandia
The Pripyat Trough, representing the northwestern end of the Pripyat-Dnieper-Donetsk Basin, is located in the junction zone of the Precambrian terrains of Fennoscandia and Sarmatia, controlled by the Osnitsk-Mikashevichy Igneous Belt. The ancient tectonic suture was reactivated during subsequent epi...
Збережено в:
Дата: | 2020 |
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Автори: | , |
Формат: | Стаття |
Мова: | rus |
Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2020
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Теми: | |
Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/215073 |
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Назва журналу: | Geofizicheskiy Zhurnal |