Fig. 8From: Triassic radiolarite and carbonate components from a Jurassic ophiolitic mélange (Dinaridic Ophiolite Belt)Microfacies characteristics of the Late Triassic grey cherty limestones. All samples are from the Radoševo area. a Middle to Late Norian radiolarian wackestone to packstone. Sample SRB 489. Width of the photo: 0.5 cm. b Middle Early Norian filament limestone with radiolarians. The filament layers occur as turbiditic intercalations in radiolarian wackestones. Sample SRB 557. Width of the photo: 1.4 cm. c Earliest Early Norian radiolarian wacke- to packstone. Sample SRB 565. Width of the photo: 0.5 cm. d Marly radiolarian and filament layered wackestone below SRB 565, most probably Carnian. Sample SRB 564. Width of the photo: 0.5 cmBack to article page