In Donbas, Carpathians, Crimean mountains, and on the Ukrainian shield, the wide distribution of tectonites of the laramian (Late Mesozoic - Early Cenozoic) age is established. They have north-north-west vergence, which is steady in the area. Tectonic movements of this age are directed from the modern water area of the Black Sea. The composition of tectonites depends on that of containing rocks and the intensity of dynamometamorphic transformations.

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