“…This electrical resistivity, measured by comparing the electric field's horizontal component to the magnetic field on the surface, can detect a depth of several tens of kilometers associated with the acquisition frequency. With the rapid advancement in magnetotelluric modeling and inversion, it has become one of the essential tools for recognizing deep geological structures (Unsworth, 2010;Avdeeva et al, 2012;Azeez et al, 2017;Nagarjuna et al, 2021) and geophysical investigations, such as geothermal exploration (Barcelona et al, 2013;Patro, 2017;Tarek et al, 2023), mineral deposit exploration (Benjamin et al, 2018;Jiang et al, 2022), and gas exploration (Zhang et al, 2014).…”