Late Precambrian and Paleozoic deformations of eastern part of Bashkir Anticlinorium (Southern Urals)
Structural evolution of Bashkir anticlinorium was studied on the basis of structural analysis. Two main stages, e.g. Late Precambrian and Paleozoic were determined in the structural history of the region. Precambrian stage is established according to the style of deformation holomorphic polyphase type of folding which differs radically from fault contact type of folding in Paleozoic complexes. Vendian age of dislocations (Timan Orogeny) is identified due to the presence of pre-Paleozoic unconformity, Vendian molasses and to dating of metamorphism (600-550 Ma).