Abstract
An effective method of boundary integral solution of potential problems was adopted for the solution of a direct-current geoelectric problem for a two-dimensional perturbing body embedded in the superficial layer of a two-layer model of Earth. The method is based on the combination of the boundary integral equation method (BIE) for double-layer density distribution and the Fourier transform (FT) of the potential field along the strike axis of the perturbing body. Numerical results give isolines and profile curves of apparent resistivity on the surface of the Earth for a 2-D prism embedded in the first layer. Special attention is given to the case of the outcropping body.
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