A magnetoteluric method for the geophysical exploration of the subsoil or soil under water. (Machine-translation by Google Translate, not legally binding)

摘要

A magnetotelluric method for the geophysical exploration of the subsoil or soil under water, in which only natural or erratic currents are used, excluding any artificial current generated for this purpose, characterized by the fact that the linear relationships exist between the horizontal components The electric and magnetic fields are first determined, after which said relations are interpreted applying the laws of electromagnetism in order to deduce from these quantitative information about the constitution of said soils. (Machine-translation by Google Translate, not legally binding)