The different aspects of fracturing at sedimentary series of orogenic belt in connection with reservoirs structure are viewed. Integrated assessment on geology, geomorphology, tectonophisics, geophisics, geochemistry, petrophisics, field data and core analysis show the most common feature of fracturing in the Middle Ural`s frontal folds. Mass measurements of lineament orientation were used to constract rose diagrams and stereographic projections that characterize fracturing reservoirs.