Finite Element Method for Modeling 3D Resistivity Sounding on Anisotropic Geoelectric Media

Figure 14

(a) A 3D anisotropic cube in a homogeneous isotropic half-space. The principal resistivity of the cube is given by = 10/10/100 Ω⋅m and the background resistivity is 100 (Ω⋅m). (b) 21 survey lines were deployed along both - and -direction and the solid lines outline the boundary of the buried cube.

(a)

(b)