## 1 Introduction  
The study of modern geodynamic processes employs non-destructive methods in analysis of the physical parameters associated with the time variation of the stress-strain state (SSS) of geological media, specifically the lithosphere. Non-destructive methods mostly use on-surface monitoring tools based on remote response, like magnetotelluric sounding (MTS). This analysis is crucial for field assessments of earthquake-generating fault monitoring, which holds high priority in engineering geology, geotechnics, and geotechnical earthquake engineering. Geological rocks are microscopic heterogeneous media, where pores, cracks, inclusions, and mineral grains act as inhomogeneities at various spatial scales. However, the observed physical properties of rocks are macroscopic, as per the theory of microscopic heterogeneous media. Changes in macro anisotropic parameters are linked to irreversible deformations occurring within the Earth's crust [1,2]. Electromagnetic monitoring is one of the geophysical methods employed to study these processes. By utilizing controlled sources of electromagnetic fields and describing the fractured rock as a bianisotropic medium, new effects can be observed, including exceptions to the electromagnetic reciprocity transfer (ERT) principle. \"The complex interpretation of the fracture system studied can provide direct inputs for hydrogeological models, but can also provide conceptual information for the development of the geosphere module in safety calculations.... The stochastic fracture network models are often accompanied by only a few large-scale features (faults, deformation zones) that are important enough to be modeled deterministically\" [3]. Continuous geophysical monitoring of modern geodynamic processes is a highly successful technological approach for analyzing incoming geological and geophysical information with the aim of advancing theory and preventing global natural disasters. It is a frontier of the modern epoch in testing the environment [4]. Electromagnetic monitoring of the Earth's crust in seismically hazardous regions constitutes a fundamental area of research. It enables not only the monitoring of geodynamic processes in the Earth's crust but also theoretical development and assessment of the physical parameters of the geological media. Geophysical monitoring has become an indispensable tool for studying the development and current state of geodynamic processes. Electromagnetic monitoring, including both water areas and land-based monitoring, including wells, plays a crucial role in this regard. The purpose of this study is to investigate the relationship between modern geodynamic processes in the Earth's crust through the distribution of the macro anisotropic properties of rocks variations and establish a theoretical basis according to EMA for further investigations. Modern geodynamic processes involve vast rock masses and result in the ordering or disordering of rock structures within large geological formations. This, in turn, affects the effective electrical parameters of these formations. Since it is impractical to physically or experimentally model the influence of powerful geodynamic processes on the physicoelectric properties of rocks, mathematical modeling becomes crucial in determining effective petrophysical characteristics. Typically, rock masses are characterized by factors such as connectivity, size, orientation, or fractures. When drilling, \"a flow in the fracture system in a 3D rock volume while structural data (borehole images, outcrops, etc.) describe the static components (orientation, intensity, spatial model, etc.) of the fracture system\" [3] is used. Fracture parametrization (geometry of fracture networks in crystalline rocks) and the anisotropy of the system and its electrical conductivity have been extensively studied [5]. To account for various geological factors, it is necessary to establish a rigorous physical model of the rock with an appropriate mathematical formulation.