Electrical Tomography Software
Res3dinv - PASI srl
In areas with complex geology, there is no substitute for a fully 3D surveys. The arrays supported include Pole-Pole, Pole-Dipole, inline Dipole-Dipole, equatorial Dipole-Dipole, Wenner-Schlumberger and also non-conventional arrays.
RES3DINV uses the smoothness-constrained least squared inversion technique to produce a 3D model of the subsurface starting from the data of apparent resistivity.
