BERICHTE DES INSTITUTES FÜR GEOLOGIE UND PALÄONTOLOGIE DER KARL-FRANZENS-UNIVERSITÄT GRAZ, ÖSTERREICH
Abstract
An overview of the geological evolution of the Carnic Alps during the Palaeozoic is presented: the Variscan sequence, the Permo?Carboniferous sequence and the basal part of the Alpine sequence were deposited between the Late Ordovician and the Middle Triassic.
