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The aim of this study was to determine properties of the tectonic contact between Permian/Mesozoic limestones\udand less competent Miocene clastites on the northeastern foothill of the Boč Mt. Because fault planes signifiantly\udmark the relief, this contact was studied by a detailed structural mapping, which showed that the Boč Mt. is\udlimited by subvertical faults in its northeastern part. To ensure that mapped subvertical contact is compatible\udwith regional geodynamics of the area, additionally paleostress analysis of fault-slip data was performed. Four\udindividual paleostress tensor groups were documented in a wider Boč area and compared by published structural\uddata from the border zone between Alps, Dinarides and Pannonian Basin. The oldest paleostress tensor group\ud(Phase 1) is likely of Lower and Middle Miocene age and indicates SW-NE extension accommodated by W-E to\udWNW-ESE striking normal faults. Phase 2 can be correlated with Middle to Late Miocene NW-SE to WNWESE directed extension accommodated by NNE-SSW striking normal faults. Phase 3 is correlated with Late\udMiocene W-E directed contraction accommodated by N-S striking sinistral faults and NNE-SSW to NE-SW\udstriking dextral faults. The youngest paleostress tensor group (Phase 4) fis well with Pliocene to Quaternary\udNNW-SSE to N-S directed contraction accommodated by NW-SE to W-E striking dextral faults and NE-SW\udstriking reverse faults. Since the documented paleostress phases fis well with the geodynamic processes of the\udAlps-Dinarides-Carpathians territory the subvertical border in the northeastern part of Boč Mt. seems to be\udan acceptable structural solution. The study is important because the study area is located at interaction zone\udbetween two major Alpine fault systems: the Periadriatic and the Lavanttal faults

A contribution to better understanding of structural characteristics and tectonic phases of the Boč region, Periadriatic Fault Zone