Fig. 4
From: Middle Jurassic limestone megabreccia from the southern margin of the Slovenian Basin
Composition of limestone breccia lithoclasts that derive from platform margin limestones: a polished surface of boundstone sample with Norian-Rhaetian coral Retiophyllia fenestrata Reuss and chaetetid Atrochaetetes cycliformis Bojko; b Norian-Rhaetian reef limestone lithoclast composed of chaetetid frame-builders (F), calcimicrobic encrusters (E), and cement (C) (thin-section was made from the sample in Fig. 4a); c Norian-Rhaetian bioclastic rudstone lithoclasts with large fragmented frame-builders and other bioclasts (in boxed area foraminifer Miliolipora tamarae Gale, Rettori & Martini is enlarged) and partly dolomitized intraclasts (indicated by arrow); d Rhaetian partly-washed pelletal bioclastic packstone lithoclast with foraminifer Triasina hantkeni Majzon; e Lower Jurassic pelletal bio/intraclastic grainstone lithoclast with foraminifer ?Lituosepta recoarensis Cati and micritized ooids (peloids)