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164 Ślączka A. et al.

Fig. 13 - Facies Association E (lower shoreface zone with bar system). Area between Torretta and Bue Marino. a) Lower part of the As-
sociation E. Sequence started by fine-grained calcarenites (FC) followed by subhorizontal laminated calcarenites (H and set of bi-
directional cross-bedded calcarenites covered by horizontal layers coarse grained calcarenites partly pervasive bioturbated (B). Cross
lamination is inclined to S and NW. That sequence show resembles to Facies Association C. Punta Marsala; b) Lower part of Facies
Association E. Sequence started with parallel laminated calcarenites (L) overlaid by cross-bedded zone (T) that have oblique to sigmoid-
al stratification facing SW (shoreward), and terminated by set of medium scale trough cross-bedding (B) resembling hummocky cross-
bedding, with bioturbated horizons. Note flat dunes. Probably crest or landward slope part of an outer bar. Cliff in Calarossa; c) Detail of
Fig. 12a that show internal architecture of cross-bedded facies. Note the diminishing inclination of cross-lamination on lee side of dunes
(white arrow); d) sequence of medium to large-scale bi-directional tabular cross-bedding calcarenite bodies. Bue Marino; e) synsedimen-