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.
Geology and stratigraphy of the Cason di Lanza area (Mount Zermula, Carnic Alps, Italy)
CORRADINI, CARLO;CORRIGA, MARIA GIOVANNA;
2012-01-01
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:
Non ci sono file associati a questo prodotto.
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
