Abstract
Tectonic contact between Paleozoic and Triassic rocks south of Podolseva, which passes prominent cliffs over the left bank of Savinja river (Klemenca pec, Jamnikova pec, Golerjeva pec, Strevceva pec and Huda pec), 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 Podolsevski prelom (Podolseva fault).
Highlights
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
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
Severno od pasu triasnih kamnin so prete‘no paleozojski, spodnjekarbonski klastiti, vmes pa so redki vlo‘ki prav tako spodnjekarbonskih laminiranih apnencev, ki nastopajo v obliki le~ in dose‘ejo najve~jo debelino do okoli 40m
Summary
Tektonski stik med paleozojskimi in triasnimi kamninami ju‘no od Podol{eve, ki poteka po zna~ilnih pe~inah nad levim bregom Savinje (Klemen~a, Jamnikova, Golerjeva, Strev~eva in Huda pe~), je po rezultatih novega kartiranja prelom, ki strmo vpada proti severu. V zadnji fazi je bil prelom desnozmi~no aktiven, v prej{njih pa je bil verjetno tudi reverzen. Predstavlja lahko spremljajo~o strukturo Periadriatskega lineamenta, nastal je v transpresivnemu re‘imu in ustreza modelu izrivne strukture (pozitivne strukture ro‘e).
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