Applications in Geological Identification
Each type of rock magnetizes according to its magnetic susceptibility, influenced by the amount and distribution of magnetic minerals present. This concentration of minerals creates distortions in the Earth’s magnetic field, detectable and capable of providing valuable information about the subsurface.
In addition to locating economically relevant magnetic minerals, magnetic measurements can identify geological contacts, structures such as faults or folds, and, by geological association, even non-magnetic minerals such as chalcopyrite, galena, and chalcocite.
After a magnetometric data acquisition campaign, corrections are performed, including the removal of spurious measurements (spikes), diurnal correction and removal of IGRF.
In the processing of magnetometric data, various products will be generated from the derivations of the anomalous magnetic field (CMA) and the 2D/3D inversions/modeling, resulting in valuable products for interpretation.