MAPPING NEARLY VERTICAL DISCONTINUITIES BY EARTH RESISTIVITIES
Following a procedure similar to the method used by Stefanesco et al. (1930) in resistivity computations for a horizontally bedded earth, integral formulas are evaluated for the potential distribution around one current electrode placed in the neighbourhood of (a) one vertical plane of discontinuity and (b) two vertical planes of discontinuity. The integral formulas are shown to be identical to the series evaluated by Hedström (1932) using a Maxwell theory of images. The apparent resistivity in the one‐current‐electrode configuration is defined, and integral formulas are given for planes of discontinuity. Because the evaluation of apparent resistivity curves across a gangue of small thickness is troublesome by these formulas, approximation formulas for a thin vertical sheet are evaluated, these are found to be of sufficient accuracy in most cases met in the field. It is suggested that nearly vertical faults, rock boundaries, and breccias in many cases give geoelectrical anomalies which can be assumed to be caused by vertical planes of discontinuity. As an example, resistivity data are presented which were taken across a breccia in Meheia, near Kongsberg, Norway.