Abstract
In accordance with the data of tectonophysical studies of a set of uranium deposits of the central part of the Ukrainian shield it was shown that those deposits were formed on the stage of compression of the Earth's crust between two stages of stretching. The stretching prevented through passage of ore solutions to the day surface above the surface of erosion. In this case the structures of uplifts type with hanging flanks that served as a screen for ore solutions were formed. Ore mineralization was mainly concentrated in ruptures with oblique bedding (thrust faults) and were kinamatically conjugated with thrusts.
Highlights
In accordance with the data of tectonophysical studies of a set of uranium deposits of the central part of the Ukrainian shield it was shown that those deposits were formed on the stage of compression of the Earths crust between two stages of stretching
The stretching prevented through passage of ore solutions to the day surface above the surface of erosion
In this case the structures of uplifts type with hanging flanks that served as a screen for ore solutions were formed
Summary
In accordance with the data of tectonophysical studies of a set of uranium deposits of the central part of the Ukrainian shield it was shown that those deposits were formed on the stage of compression of the Earths crust between two stages of stretching. Íîâîêîíñòàíòèíîâñêàÿ çîíà ñêàëûâàíèÿ àíàëîã Áîáðèíåöêî-Æåâàíîâñêîé, îäíàêî, ïîñêîëüêó îíà íàõîäèòñÿ âíå ïðåäåëîâ Êèðîâîãðàäñêîé çîíû ðàçëîìîâ, ôàçà äåôîðìàöèè, ñ êîòîðîé ñâÿçàíà ýòà çîíà ñêàëûâàíèÿ, íàçâàíà åå ñîáñòâåííûì èìåíåì [Ãèíòîâ, Ìû÷àê, 2011 á].
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