деформаційна фаза

Reconstruction of cenozoic paleostress fields in the flysch complex of the Opir river valley (Skyba nappe, Ukrainian Carpathians)

Purpose. Reconstruction of paleostress fields, as evidence of many publications of different parts of the Carpathians, can carried out through research the most common brittle and semibrittle structure – joints, slickensides, faults, regional and local folds, or complex research of joints and slickensides. The purpose of this paper is to reconstruct the paleostress fields and deformation regimes of flysch deposits in Opir River Valley using complex analysis of joints and slickensides.