n this paper researches of different methods of geophysical data interpretation on the example of the Republic of Bashkortostan were made. According to initial data a map of the admittance as the ratio of anomalies of gravitational and magnetic fields was compiled. Modeling the geomagnetic and gravity data has greatly clarified the structure of the studied area. The simulation results do not contradict geological concepts and provide an opportunity to assess their zonal distribution. Detection of such zones indicates intense dynamics and wide development of magmatic processes in fault-block platform crust in the region. The analysis of the data showed the relationship between the location of the epicenters of regional earthquakes and the line of maximum values of admittance. In addition, there is an evident correlation between the sizes of admittance: in large areas, the magnitude of earthquakes is higher than in areas where admittance is less tracked. Thus, the obtained results show the possibility of using the method of admittance as an additional parameter to highlight the areas of geodynamic risks.