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Tectonic contact between Paleozoic and Triassic rocks south of Podol{eva, which passes prominent cliffs over the left bank of Savinja river (Klemen~a pe~, Jamnikova pe~, Golerjeva pe~, Strev~eva pe~ and Huda pe~), is on the basis of the new mapping a steep fault, dipping to the north. In the last phase, the fault was dextral strike – slip active, before was probably reverse, and can represent accompanying structure of Periadriatic lineament. It was under transpresive tectonic regime and complies with model of positive flower structure. We named it Podol{evski prelom (Podol{eva fault). doi:10.5474/geologija.2002.030

Tectonic contact beetwen Paleozoic and Triassic rocks south of Podolševa (Slovenia)