It permits to detect conductors as deep as 150 and to specify their physical properties through the use of an extended range of up to 10 frequencies (110 – 14 080 Hz) and variable transmitter-receiver separations.
Geophysical technique that provides information about the distribution of electrical conductivities of underground rocks. This is a method of electromagnetic exploration where electric currents, of natural and artificial origin, continuously scour the basement. Their variations induce magnetic fields which can be detected on the surface. The magnetotellurics are particularly suitable for search of metal ores and study of geothermal sites and hydrocarbons.