PMH-1, Javorniški Rovt, the western Southern Karavanks.
Trogkofel Formation (upper part)/Goggau Limestone?
Back-reef or back-bank lagoon with well-lit, well-agitated shallow water indicated by dasyclads and Osagid grains.
Fenestral bioclastic peloidal grainstone with dissolution void containing apparently suspended Tuberitina benthic foraminifera tests surrounded by radial fibrous (prismatic?) cement, which darkens under the cross nicols, forming pseudouniaxial cross.