Fig. 2

Geological map and cross-section of the Rute Plateau area: Ladinian basinal succesions (green and blue colors) are located in the northwestern part of the area, while the eastern and southern parts are dominated by platform carbonates (yellow and orange colors). The transition between the sedimentary environment end members is characterized by paleotectonic blocks dominated by platform carbonates, but also containing intervals of basinal deposits. Facies transitions are rapid and occur along faults (bolded) considered to be synsedimentary