деформації порід

In the paper the history of development and methodical-apparatus supply and results of extensometric observations in the Beregovo hills area in Transcarpathians in particular in Mujievska (Grand Beregivska) mountain is shortly described. The method of separation and results of analysis of deformation anomaly – precursor of perceptible 1989 Vynogradovo earthquake is given. The changes of geomechanical regime of Mujievska mountain rocks massifs till and during and after this earthquake are traced.

Purpose. The aim of the work is to present and to analyze the results of physical modeling and field studies of processes of formation, evolution and modern geodynamic and seismotectonic activity of subvertical shear zones (SVShZ), in particular of faulting kinematics. Methods. Physical modeling was conducted on the special modeling machine for break dip angle 75, 60 and 45. As a plastic-viscous modeling materials for this were used a special paste which are based on clay. Field researches included geoacoustic emission, PIEMPZ, extenzometric, tiltmetric and seismological methods.

Purpose. The aim of the work is to present and to analyze the results of physical modeling and field studies of processes of formation, evolution and modern geodynamic and seismotectonic activity of subvertical shear zones (SVShZ), in particular of faulting kinematics. Methods. Physical modeling was conducted on the special modeling machine for break dip angle 75, 60 and 45. As a plastic-viscous modeling materials for this the special pastes were used which are based on clay.