The present work implements the interdisciplinary approach that combines the methodology of solid mechanics and geomechanics with tectonophysical analysis. Solutions derived from geomechanical modeling based on elastic-brittle-plastic models of rocks are presented in the form of spatial distributions of stress-strain parameters. The analysis and interpretation of the obtained results within the framework of tectonophysics leads to the conclusion that local tectonics affects the distribution of dip slip faults along the sides of feathering faults during the stick-slip displacement in the basement. In this work, the procedure of tectonophysical analysis is described by the example of numerical modeling of the formation of a flower structure. Estimates are obtained for the kinematics of faults.