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...
Gespeichert in:
| Datum: | 2020 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | rus |
| Veröffentlicht: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2020
|
| Schlagworte: | |
| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/215073 |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| Назва журналу: | Geofizicheskiy Zhurnal |