Trabia and Termini-Imerese Hydrogeological Basin
摘要
The Trabia and Termini Imerese mountains fall in the northern sector of the northern Sicilian chain (Fig. 11.1) and are the result of the tectonic superposition of various carbonate, carbonate-silicoclastic and terrigenous geological bodies, of Upper Triassic–Lower Miocene age, with generally southern vergence. These bodies derive from the Miocene deformation of a pelagic basin and escarpment succession (Dominio Imerese Auct.), formed during the Mesozoic distensive phases, crowned by silicoclastic terrigenous deposits (Fysch Numidico Auct.).