Use of Different Frequencies of ENPEMF Method for Determination of Different Deep Fractures

Abstract

The application results of the measurement method of the Earth's natural pulsed electromagnetic fiel (ENPEMF) for the study of tectonic fault zones on the territory of Ivano-Frankivsk. The subject of research was not chosen by chance, as there are several known tectonic fault zones and their locations on the territory under study. The anisotropy factor is the most informative; it eliminates anomalies of obstacles (interferences) and enhances real anomalies of geological objects. It was also proved that different frequencies of electromagnetic field carry information from different depths: low frequency – large depth study, high frequency – low depth study.