Fig. 4

Spatial distribution of the four tectonic paleoblocks (top) with generalized successions (bottom), and location of the detailed sedimentological logs (A—Črna voda, B—Kobilji curek, C—Vrh, D—Podlaz, E—Potok pri Mohorju – for details see Additional file 1). Paleoblock 1 is in the NW is dominated by basinal facies (F1, F2 and F3) with two intervals of platform carbonates (F4), paleoblocks 2 and 3 are dominated by platform carbonates (F4) with intervals of basinal facies (F1, F2 and F3), while paleoblock 4 in the SE contains exclusively platform carbonates (F4) (Line X–Y marks the position of Fig. 5 schematic cross-sections)