Fig. 5 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf

Fig. 5. Field photo of studied eastern quarry at Śluchowice (A; see Figs. 2, 9), with close−up of very−thin bedded Śluchowice Marly Level, showing initial slump folds and flat pebbles (B; scale bar 20 cm; compare with Szulczewski 1968: fig. 2).