BERICHTE DES INSTITUTES FÜR GEOLOGIE UND PALÄONTOLOGIE DER KARL-FRANZENS-UNIVERSITÄT GRAZ, ÖSTERREICH
Abstract
In the Nassfeld area the post-Variscan sequences of the Carnic Alps is well preserved and consists of Late Palaeozoic to Early Mesozoic units which were deposited in equatorial realms. Of them the lithological and stratigraphical characteristics of the
Carboniferous to Permian sediments are briefly described.
