These terranes show a Late Oligocene HP/LT followed by green schist facies metamorphism. The ophiolite-bearing units are unconformably covered by turbiditic synorogenic sequences (Saraceno fm and Cilento group),
representing perched basin deposits (Fig. 5).
Figure 4 – Geodynamic and regional geological framework of southern Italy (from Mazzoli et al., 2000; Iannace et al., 2007).
Figure 5 – Tectono-stratigraphic representation of the northern Calabria and Southern Apennines (Pollino Massif) mountain belts (from Critelli, 1993).
