“…The Cartesian components of the dipoles approximating the sample are estimated by iteratively solving a large linear inverse problem. This method is an adaptation of the well‐known equivalent layer technique, which has long been applied to processing potential‐field data in space domain [ Dampney , ; Emilia , ; Von Frese et al ., ; Hansen and Miyazaki , ; Silva , ; Leão and Silva , ; Cordell , ; Mendonça , ; Mendonça and Silva , ; Guspí and Novara , ; Li and Oldenburg , ; Barnes and Lumley , ; Oliveira Jr. et al ., ; Kara et al ., ; Li et al ., ; Barnes , ]. The study developed by Weiss et al .…”