The method of defining the stone deformation by quantitative correlation of fracture distribution, with the aim of determining the distribution of fractures in the same rocks and different time of formation at different survey sites for the purpose Solving the inverse problem with input data is a measure of the fracture potential obtained from rocky outcrops in the field, to aid in the identification of rock deformation phases. This method consists of the following main steps: B1: Use the site to collect positional measurements (azimuthal slope and slope angle) of each fractured surface in the field. B2: Enter the coulometric values ​​obtained in the software to draw them on Schmidt's hemispherical projection grid and determine their occurrence at each rocking point. B3: Quantitative correlation of fissile substitutents located between the openings on rocks of the same age and different age in the area. Determine the rock deformation phases (if the correlation coefficient is between ≥70%, they are considered to be the same deformation phase).