O startygrafii i paleogeografii kajpru wierchowego w Tatrach

Abstract

STRATIGRAPHIC AND PALAEOGEOGRAPHIC PROBLEMS IN THE HIGH-TATRIC KEUPERMarked facial differentiation has been recorded within the high-Tatric Keuper series. Denudation has been at work in many places during the Carnian. The shaly-conglomeratic facies was predominant then while during the Norian dolomites of considerable thickness formed too. Previous to the Lias but after the Keuper distinct traces of orogenic movements on no great scale were observable within the high-Tatric series.