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Deep Structure and Geodynamics of the Sarmatia–Fennoscandia Transition Zone

The geological structure of the crust and mantle within the transition zone between the Sarmatia and Fennoscandia miniplates, which encompasses the central and southern parts of the Svecofennian orogen and the northwestern segment of the Ukrainian Shield was examined. The transition zone is extended...

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Datum:	2026
Hauptverfasser:	Gintov, Oleg, Mychak, Sergii, Babynin, Oleksii
Format:	Artikel
Sprache:	Englisch
Veröffentlicht:	S. Subbotin Institute of Geophysics of the NAS of Ukraine 2026
Schlagworte:	Sarmatia Fennoscandia Svecofennian orogen Ukrainian Shield transition zone mantle subduction
Online Zugang:	https://journals.uran.ua/geofizicheskiy/article/view/344412
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Назва журналу:	Geofizicheskiy Zhurnal

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