1. The influence of electrical anisotropy on mise à la masse surveys;Asten;Geophys. Prospect.,1974
2. A method for calculating mise-à-la-masse anomalies in the case of high conductivity contrast by the integral equation technique;Eloranta;Geoexploration,1984
3. An equipotential conductor in a homogeneous, anisotropic half-space, an integral equation formulation for the modelling of geophysical direct current anomalies;Eloranta;Helsinki University of Technology, Department of Materials Science and Mining, Laboratory of Economic Geology, Research Reports TKK-TGE A6,1987
4. Addendum to “The solution of the stationary electric field strength and potential of a point current source in a 212-dimensional environment” by L. Eskola and H. Hongisto;Eskola;Geophys. Prospect.,1984
5. The solution of the stationary electric field strength and potential of a point current source in a 212-dimensional environment;Eskola;Geophys. Prospect.,1981