The Julian and Tuvalian lithologic column in the Oslica area starts with dolomitic breccias with limonitic groundmass and with a bauxite giving evidence of areal expose on the boundary between Cordevolian and Julian.Afterwards, precepitation of carbonate fr8608 rocks followed.In the lithological interval where the limestone breccias predominate, oncolitic horizons are most characteristic.The Carnian sedimentary succession in the Oslica is terminated by a dolomite with intercalations of marls, bedded micritic limestones and a darkgrey dolomite with a roundish disintegration.
The lithological composition and sedimentological characteristics of the 2004 bmw 325i hood succession indicate an origin in the littoral environment.