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304 R. Catalano et al./ Tectonophysics 260 l 1996) 291-323
ern margin of the Madonie Mountains and Nebrodi by younger E-W-trending thrusts that also offset
Mountains, in northem Sicily, the tectonic contacts Messinian-Lower Pliocene rocks (Figs. 2 and 7;
between Sicilide and Numidian Flysch are modified Ghisetti and Vezzani, 1984; Abate et al., 1993).
NW SE
0•,---------------------------------------------------------------------------------------,
NW SE
Os,-------------------------------------------------------------------------------------,
Fig. 13. Maghrebian-Sicilian lnner Carbonate TS. The seismic section shows from the top: roof complex of terrigenous successions,
inferred to be Numidian Flysch, overlying a duplex wedge of interpreted basin-type carbonates, in tum overthrust on carbonate platform
units. Key: M - Messinian horizon; FN - Numidian Flysch; Tb - top of basinal successions; Tp - top of platform carbonates.

