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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Bibliographic Details
Date:2026
Main Authors: Gintov, Oleg, Mychak, Sergii, Babynin, Oleksii
Format: Article
Language:English
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2026
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Online Access:https://journals.uran.ua/geofizicheskiy/article/view/344412
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal