Alicante, España
Urbino, Italia
Nápoles, Italia
The Tertiary of the Stilo Unit (Internal Calabro-Peloritani Zone) is studied. Two sedimentary cycles are distinguished (pretectonic ans syntectonic, respectivelly). The pretectonic cycle is divided into two depositional sequences (Early Oligocene and Late Oligocene-Aquitanian in age). The syntectonic cycle is restricted to an Early-Middle Burdigalian age. This framework is correlated with the Tertiary of the Morron de Totana Unit (Malaguide from the Internal Betic Zone) and similities in stratigraphy, age and geodynamic evolution have allowed us to propose a close paleogeographic origin and a parallel tectonic history, for both units.
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