Magnetotellurics (MT) is a geophysical method used to investigate the electrical conductivity structure of the Earth’s subsurface using natural electromagnetic (EM) fields. It relies on measuring naturally occurring electric and magnetic fields at the Earth’s surface and analyzing their variations to infer subsurface resistivity, which can be correlated with geological structures and the presence of fluids
Combines the strengths of both techniques to improve near-surface subsurface imaging, achieving high-resolution models and overcoming the limitations of individual methods.
Combines the strengths of both techniques to improve near-surface subsurface imaging, achieving high-resolution models and overcoming the limitations of individual methods.
Combines the strengths of both techniques to improve near-surface subsurface imaging, achieving high-resolution models and overcoming the limitations of individual methods.
A powerful petrophysical modeling tool that uses genetic code designed to estimate mineral and fluid compositions in the most complex geologic environments
A powerful petrophysical modeling tool that uses genetic code designed to estimate mineral and fluid compositions in the most complex geologic environments