Fig. 3
From: Middle Jurassic limestone megabreccia from the southern margin of the Slovenian Basin
Composition of limestone breccia lithoclasts: a lithoclasts derive from diverse sedimentary environments and are predominantly limestones (upper left—ooidal grainstone, upper middle right—“resedimented packstone”, right—pelagic wackestone, lower left—chert); b early Middle Jurassic pelagic wackestone litho/intraclast (arrow points to planktonic foraminifer Protoglobuligerina sp.); c pelagic packstone lithoclast composed of thin-shelled bivalves and ammonites; d coarse bioclastic wackestone lithoclast with echinoderms, foraminifera, sponge spicules, and mollusks; e bioclastic grainstone lithoclast composed of echinoderms and rare intraclasts (in boxed area foraminifer Involutina liassica Jones is enlarged); f ooidal wackestone lithoclast with thin-shelled bivalves