J. Cincura, OLD PALEOKARST PLATEAUS ON THE EASTERN MARGIN OF THE VIENNA BASIN (MALE KARPATY MTS., SLOVAKIA), Zeitschrift fur Geomorphologie, 42(2), 1998, pp. 255-263
One of the typical features of the Male Karpaty Mts. are extensive lev
elled paleokarst plateaus. They are developed on carbonate sequences (
limestones and dolomites) of Middle and Upper Triassic age and collaps
e breccias of the Upper Cretaceous. The Upper Cretaceous-Paleocene kar
at period was interrupted by the Eocene marine transgression. Karst pr
ocesses were probably reactivated as early as in the Miocene.