In this paper, a correlation between magnetic data and geology of research area is given and it enable adequate geological explanation. Nevertheless, we managed to separate large geological units within the investigation area by modelling of geomagnetic measurements. On the current level of investigations and on the basis of current knowledge, we assumed the position of the regional fault and lithological boundary of two regional geological units. The obtained results does not give possibility of quantitative interpretation, because we need data of other geological and geophysical investigations (susceptibility measurements, detailed geological mapping, gravity method...) for such interpretation. In that sense, these results stay in the domain of qualitative interpretation. Results show very good correlation between geomagnetic data and data of geological mapping and the measured elements of tectonic fabric.
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