Based on sedimentological features and faunal associations, the following facies associations have been identified: 1) Marls and limestone with terrigenous clasts; 2) Build-ups with tubular/massive corals and rudists; 3) pillarstone-type bioaccumulations with branching/platy corals; 4) bioclastic rudstone/grainstone; 5) bioclastic floatstone/packstone. All these facies associations indicate a coastal environment developed along a shelf margin influenced by both the terrigenous supply, and the relative sea level
variations.