Disruptive dislocations of the Preduralie Nature Reserve

Abstract

The study of the geological structure and lithological-facies analysis of the deposits of the Pre-Ural reserve made it possible to identify fault dislocations associated with the Suksun fault. X-ray fluorescence and X-ray phase analyzes of loose sediments in the Klepovsky Log fault zone indicate processes of leaching, hydrolysis and authigenic mineral formation in the form of iron hydroxides and illite as a result of exposure to low-temperature hydrothermal solutions.