Abstract
The solution of forward 2-D geoelectric problems is considered for anisotropic and bianisotropic media. The problems are reduced to the solution of integrodifferential equations obtained with the use of integral Fourier and Fourier-Bessel transforms for horizontally heterogeneous layered media and radially heterogeneous layered media. This approach is particularly effective for studying the influence of small-scale geological structures (such as faults, borehole wall mud cakes, and the like) on results of geoelectric studies.
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