MAIN FEATURES OF THE PRE-GOSAU PALEOKARST IN THE BREZOVSKE KARPATY MTS. (WESTERN CARPATHIANS MTS., SLOVAKIA)

Rok, strany: 1998, 297 - 300

The considerable areal extent and a great thickness of Middle/Upper Triassic carbonate sequences favourably influenced the development of paleokarst during the Paleoalpine karst period in the Brezovske Karpaty Mts. Carbonate formations provide data concerning the first-pre-Gosau-phase of the Paleoalpine karst period. Freshwater limestones, bauxites, reddish ferrugineous silty clays, Valchov Conglomerates, shallow doline-like depressions and deeper canyon-like forms represent the most important pre-Gosau karst sediments and forms.

ISO 690:

Cincura, J. 1998. MAIN FEATURES OF THE PRE-GOSAU PALEOKARST IN THE BREZOVSKE KARPATY MTS. (WESTERN CARPATHIANS MTS., SLOVAKIA). In Geologica Carpathica, vol. 49, no.4, pp. 297-300. 1335-0552.

APA:

Cincura, J. (1998). MAIN FEATURES OF THE PRE-GOSAU PALEOKARST IN THE BREZOVSKE KARPATY MTS. (WESTERN CARPATHIANS MTS., SLOVAKIA). Geologica Carpathica, 49(4), 297-300. 1335-0552.