Geodynamics of the Azov-Black Sea coast during the period of Turkish earthquakes in February-March 2023
UDC
539.3DOI:
https://doi.org/10.31429/vestnik-20-2-18-27Abstract
The development of geodynamic processes on the territory of the Azov-Black Sea coast during the period of earthquakes in Turkey 06.02.2023 is being considered according to continuous GPS measurements. The observed movement of geodynamic stations Gelendzhik, Temryuk, Sochi and Lesnoye northwest of the trend may be caused by the increasing pressure of the Anatolian plate on the northern side of the Black Sea Depression.
After seismic events 06.02.2023 in Turkey there is a subsidence of these points in height, which indicates stress relaxation in the study area. According to the data of maximum slip rate obtained in the national network of Turkey TNPGN-Active (1.5 m and 5.2 m), the estimated magnitude of expected earthquakes in the area of ?the East Anatolian fault was 7.1 and 7.5, which is close to the values of earthquakes 7.5 and 7.8.
The estimate of the time of geodynamic activity in the studied area since the Turkish earthquakes 06.02.2023 is 8 to 80 years for the empirical model of earthquake epicenter migration and 1.6 months for the nonlinear rotational model of the seismic process, which is confirmed by the increase in seismicity in the Caucasus and the activation of mud volcanoes on the Taman Peninsula in the spring of 2023. It was proposed to use continuous observations at TNPGN-Active network stations (primarily ANTE, ONIY, MLT1 and EKZ1) for the period 2016-2023 to determine the integral criterion of crustal stress according to the methodology developed at the SSC RAS for the purpose of retrospective monitoring of geodynamic processes and early warning of seismic hazard.
Keywords:
earthquakes in Turkey, seismic activity, GNSS measurements, Azov-Black Sea coastAcknowledgement
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