Integrated geological-geophysical characterization of the zone of the Kherson—Smolensk transregional tectonic suture — deep long-lived magma- and fluid-conducting channel

The transregional Kherson—Smolensk suture has been established to be located between large meridional faults of the crystalline crust of the Ukrainian Shield (USh) in a strip of 50—70 km width and separates two microplates of different composition of the Precambrian basement. It is traced by subcru...

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Bibliographic Details
Main Authors: І. К. Пашкевич, О. М. Русаков
Format: Article
Language:English
Published: Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine 2021-11-01
Series:Геофизический журнал
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Online Access:https://journals.uran.ua/geofizicheskiy/article/view/244075
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