The schistosity of the Palaeozoic basement of the Capo San Andrea unit (Peloritan Dorsale) is cut by Liassic to Eocene neptunian dykes which developed along a pelagic fault scarp exposed on the sea bottom for 140 My. The Mesozoic structures determined the location of the Alpine deformation.
Un escarpement sous-marin permanent du Lias à l'Eocène, dans la Dorsale calcaire Péloritaine (Sicile, Italie). [A Liassic to Eocene sub-marine scarp in the Peloritan Dorsale (Sicily, Italy)]
SOMMA, Roberta;
1999-01-01
Abstract
The schistosity of the Palaeozoic basement of the Capo San Andrea unit (Peloritan Dorsale) is cut by Liassic to Eocene neptunian dykes which developed along a pelagic fault scarp exposed on the sea bottom for 140 My. The Mesozoic structures determined the location of the Alpine deformation.File in questo prodotto:
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