Structural setting
The outer portion of the Northern Apennines is bound by the Pliocene Olevano-Antrodoco-Sibillini (OAS) thrust, cropping out along the mountainous front between the Umbria-Marche mountain ridge and the Marche-Abruzzo pede-Apennines area (Fig. 3). The thrust plane has an irregular structural pattern roughly defined by frontal NW-SE and oblique NNE-SSW trending thrust ramps to the northwest and southwest of the apical zone, respectively (Fig. 4).
The OAS oblique thrust ramp (NNE-SSW trending sector) reactivated the Ancona-Anzio line (Fig. 5) that separated the Umbria-Marche pelagic domain and the Lazio-Abruzzo carbonate platform (Calamita et al., 2011; Di Domenica et al., 2012, and references therein). The Neogene kinematics of the OAS has been long debated, with special concern being given to the presence of a dextral component of shear (Castellarin et al., 1978; Salvini and Vittori, 1978; Coli, 1981; Koopman, 1983; Satolli and Calamita, 2008). Fold profiles are controlled by structural heritage. In fact, the NNE–SSW trending anticlines show a fault-bend reactivation mechanism, whereas the NW–SE trending anticlines develop with a fault-propagation shortcut (Calamita et al, 2012). The OAS thrust shows shear zones characterized by foliated fault rocks, which are produced by pressure-solution, cataclastic, and slip deformation mechanisms (Koopman, 1983;). In the NW-SE trending sector of the OAS frontal thrust ramp, SC tectonites are developed in centimeter-thick bands and show N60° tectonic transport within a simple shear-dominant deformation. Here, the S fabric is parallel to the XY plane of the strain ellipsoid. In the NNE-SSW trending oblique ramp of the OAS thrust, S-tectonites parallel to the thrust plane are characterized by a slip vector, oriented ca. N65°, within a pure shear-dominant deformation (Fig. 6). This fabric is compatible with the kinematics of the NW-SE trending sector of the OAS thrust (Calamita et al., in press).