Mathematical Problems of Seismological Monitoring of Geothermal Areas

Most of geothermal areas are located in seismically active regions. Because of an intensive tectonic regime, discontinuities of their lithosphere play the role of channels for powerful metallogenic heat and mass transfer processes, especially for intrusion of ultra-basic magmas with Fe, Mn etc. into the crust. Proceeding from the presence of substantial low resistivity structures in seismic lithosphere zones (in accordance with numerous geophysical data and the known explanation above), we derive the mathematical mo 1 of generation and propagation of seismic electro ,lagnetic and temperature signals with emission h '5 atmosphere. As a result of calculations, we give the recommendations for the seismological monitoring of geothermal areas.