Выпуск: 6 , Том: 37 , Год издания: 1996

Under consideration is a technique for transformation of a series of e.m.f. increments during electromagnetic monitoring into a series of electric conductance increments in a geoelectric section. Dynamics of electric conductance of rocks has been established at various depths. It is shown that variations of electric conductance are governed by seismic activity of the region. There are two types of anomalies in electric conductance: leading to and synchronous with a seismic event. It is established that seismic activity is correlated to varying degrees with resistivity increments at various depths.