Fig. 3From: Architecture and sedimentary evolution of the Ladinian Kobilji curek basin (External Dinarides, central Slovenia)Ladinian facies: a alternating tuff layers with different grain sizes (F1), b dark, thin-bedded limestone (F2), c pumice clasts (arrows) in thin-bedded limestone with bent laminae in underlying filament packstone (F2), d coarse limestone breccia at the base of platform limestone (F3), e fold formed by slumping in gravity mass flow carbonates (F3), f massive platform limestone (F4)Back to article page