The Upper Permian sediments from central part of the Dinarides contains three main facies: 1. carbonates (lagoonal, intertidal limestones); 2. evaporites (gypsum, anhydrite) with early-diagenetical dolomites, 3. clastic rocks (siltstones, sandstones) and one special rock type – carbonate cavity breccias. The superposing succession of three main facies types and facies of carbonate cavity breccia is often indistinct due to soil and vegetation and intensive tectonic disruption of the sequences. Evaporites are the oldest facies and are succeeded by clastic and/or carbonate facies and carbonate cavity breccias. The clastic rocks were deposited either fore-shore or playa to salt-lake playa environment. The carbonates breccias are interpretated as terrestrial features, i.e. secondary surface products of physical and chemical weathering of tectonically disrupted carbonate-evaporite sediments. Limestones of the carbonate facies occurring in association with evaporites belong to sediments deposited in restricted shallow, hypersaline lagoons or in very shallow subtidal to intertidal environments of the regressive cycle. The present surface gypsum evaporites (products of hydration of anhydrite), were deposited in evaporation conditions around the edges of an epeiric marine basin, which in conditions of a general regressive tendency and permanent coastal seawards progradation, ended in the formation and maintenance of sabkha and playa conditions.The Upper Permian evaporites of central Dinarides are comparable with evaporites from the Bellerophon Formation from the Southern Alps, Italy.