Fig. 17 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf

Fig. 17. Lateral facies and thickness variation by the transient reef retreat interval just prior to the Early–Middle Frasnian boundary in the Holy Cross Mountaints, related to Timan and Middlesex transgressive events and subsequent eustatic sea−level falls (arrowed), and regional synsedimentary tectonism, against a simplified reconstruction of the depositional environments, principally along the northern ramp−style slope of the Dyminy Reef marked by finally accelerated mud−mound growth (complementary data from Szulczewski and Racki 1981; Racki 1993b; Racki et al. 2004; Krawczyński et al. 2006; Sobstel et al. 2006). For localities see Fig. 2 (J, Jaźwica; K, Kowala; Kt, Kostomłoty; S−K, Sitkówka−Kowala; Śc, Ściegnia; Śl, Śluchowice; W, Wietrznia); GL, Goniatite Level.