STUDY OF STRESS-STRAIN STATE OF GEOLOGICAL ENVIRONMENT BY GRAVIMETRIC STUDIES OF THE FILIZCHAY PYRITE-POLYMETALLIC DEPOSIT

Abstract

Reflecting the gravitational field stress and depth dynamics of the area by gravimetric exploration, these geodynamic stress changes allowed the observation of tectonic disturbances in different depth intervals in the area and the assessment of the geodynamic regime of the area during field operation. The dynamics of the mass characterizing ∆g the anomalous areas have been shown to be active