Abstract

Summary The efficiency of the application of electrical resistivity tomography (ERT) for detailed geoelectrical mapping of near-surface geological section is illustrated by a descriptive example. The options for differentiation of the section according to electrical resistivity, provided by the method, are discussed. The application of electrical resistivity tomography in cases of presence of fissure-karst structures is demonstrated. The presented results are confirming the geological effectiveness of the discussed approach for data acquiring, analysis and interpretation.

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