In the Cason di Lanza-Mt. Zermula area rocks from Ordovician to Permian are exposed. They belong to the "Variscan sequence" and to the "Permo–Carboniferous sequence" of the Carnic Alps. The structural settings and the stratigraphic sequence of neritic and pelagic deposits are described.
Corradini C., Pondrelli M., Corriga M.G., Simonetto L., Kido E., Suttner T.J., et al. (2012). Geology and stratigraphy of the Cason di Lanza area (Mount Zermula, Carnic Alps, Italy). BERICHTE DES INSTITUTES FÜR GEOLOGIE UND PALÄONTOLOGIE DER KARL-FRANZENS-UNIVERSITÄT GRAZ, ÖSTERREICH, 17, 83-103.
Geology and stratigraphy of the Cason di Lanza area (Mount Zermula, Carnic Alps, Italy).
SPALLETTA, CLAUDIA;
2012
Abstract
In the Cason di Lanza-Mt. Zermula area rocks from Ordovician to Permian are exposed. They belong to the "Variscan sequence" and to the "Permo–Carboniferous sequence" of the Carnic Alps. The structural settings and the stratigraphic sequence of neritic and pelagic deposits are described.File in questo prodotto:
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