REFLECTION OF THE GEODYNAMIC REGIME OF THE SHAMAKHIISMAYILLI SEISMOGENIC ZONE IN LOCAL ANOMALIES OF THE GEOMAGNETIC FIELD

Abstract

According to the results of monitoring the variations of the modulus of the total vector of the geomagnetic field intensity and the spatial-temporal distributions of the magnetic field gradient conducted at the RSSC of ANAS, is considered the connection between local seismomagnetic effects and the geodynamic regime of the Shamakhi-Ismayilli seismogenic zone during the preparation and implementation of an earthquake of 05.02.2019 (ml=5.2). It is established that local magnetic anomalies reflect the stress-strain state of the earth's crust, due to the peculiarities of the geodynamic influence of faulting tectonics elements.