Fig. 2From: Middle Jurassic limestone megabreccia from the southern margin of the Slovenian BasinComposition of pack/wackestone matrix between lithoclasts: a characteristic resedimented Middle Jurassic shallow-water grains are ooids that dominate in sand-sized matrix and cm-sized oncoids; b resedimented ooids from the matrix often show bi-modal size distribution (arrow points to foraminifer Protopeneroplis striata Weynschenk inside ooid core), c matrix from Mrzli vrh section consists of fragmented thin-shelled bivalves and other bioclasts, and very rare micritized ooidsBack to article page