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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...

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Datum:	2020
Hauptverfasser:	Yegorova, Т.P., Murovskaya, A.V.
Format:	Artikel
Sprache:	Russisch
Veröffentlicht:	S. Subbotin Institute of Geophysics of the NAS of Ukraine 2020
Schlagworte:	Sarmatia Fennoscandia Pripyat Trough Korosten pluton South Pripyat fault magmatic chamber mantle degassing
Online Zugang:	https://journals.uran.ua/geofizicheskiy/article/view/215073
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Назва журналу:	Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal

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