Exploring Telluric Currents: Mapping Subsurface Resistivity
The magnetotelluric (MT) method represents a passive and electromagnetic approach to geophysical exploration, operating in the frequency domain. It consists of the simultaneous measurement, on the Earth’s surface, of the natural temporal variations of the magnetic (H) and electric (E) fields in orthogonal directions.
The objective is to map the distribution of electrical resistivity of subsurface structures at depths ranging from a few tens of meters to hundreds of kilometers..
Upon penetrating the ground, electromagnetic fields induce internal currents in the Earth, known as telluric currents, generating secondary magnetic fields. These currents originate from the magnetosphere and ionosphere, assuming that electromagnetic waves reach the Earth’s surface in the form of a flat wave. The theory of electromagnetic induction, along with related formulas, is grounded in various literary sources (Simpson, Bahr, 2005; Castells, 2006).