hrvatski

Trijaski karbonatni kompleks Papuka (izdanci uz cestu Velika–Slatinski Drenovac)

Triassic carbonate complex in the central part of Papuk Mt. is built of limestones and dolomites of Anisian and Ladinian age, outcroping along the Velika-Drenovac gravel road (Figure 1). In “Veličanka” Quarry, near Velika, Ladinian dolomites are quarried. Outcrops with Anisian lithofacies of predominantly carbonate rocks, can be observed along the road: a) folded and recrystallized crinoidal bioclastic limestones in alteration with cherts, in the lower (southern) part of the road ; and b) mainly dolomites, in the upper (northern) part of the road. Named carbonate lithology and the surrounding non-carbonate rock assemblages, together with the suitable hydrological conditions, resulted in development of karst geomorphology in this unique area of northern Croatia, apart from widely developed Dinaric Karst.

karbonati, trijas, litofacijes, krš, Velika, Papuk

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