At Capo Passero, on the southeasternmost tip of Sicily (Hyblean Plateau) a basaltic sequence is intercalated in Upper Cretaceous limestones. This rock succession is transected by a swarm of feeder dykes (84-71 Ma) trending roughly NE-SW. The basaltic dykes show the same orientation as the direction of maximum horizontal compression which has been inferred for the Late Cretaceous by the analysis of micro- and mesostructures on the coeval deep-marine carbonates (Amerillo Fm.) on the western margin of the Hyblean Plateau. Deformations within the basaltic dykes during their intrusion have been recognized by the analysis of petrofabrics. Microstructures consist of sinistral strike-slip faults trending N80°, which probably formed during the late stage of cooling of the magma. The analysis of the anisotropy of the magnetic susceptibility (AMS) highlights the primary nature of the magmatic fabric. The magnetic foliation is in fact subparallel to the walls of the dykes and corresponds to the magma flow. Locally, the Upper Cretaceous dykes are displaced up to 8 m along dextral strike-slip faults trending N110–120° which originated under a tectonic stress regime that is still active in this region, as confirmed by in situ stress measurements carried out in the neighbouring areas. The analysis of microstructures within the dykes which can be ascribed to this new deformational process shows a predominant pattern of fractures trending N120° and N140° infilled with calcite exhibiting different phases of growth. These fractures cut and displace pre-existing structures. A deeper analysis of the directions of the minimum susceptibility k 3 shows that the k 3 component is parallel to the recent shear planes cutting the dykes and fits their sense of movement. This could imply a tectonic overprinting of the magnetic fabric by the intervening recent stress field.
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