Skip to main content
Swiss Journal of Geosciences
Fig. 1 | Swiss Journal of Geosciences

Fig. 1

From: Architecture and sedimentary evolution of the Ladinian Kobilji curek basin (External Dinarides, central Slovenia)

Fig. 1

Geological setting of the study area: a location within Europe (the framed area is enlarged in b. b geotectonic subdivision of the Alps-Dinarides junction with location of the study area referred to as the Kobilji curek basin (circled capital letters mark the locations of logs shown in Fig. 6, dotted area marks the outcrops of the Slovenian Basin—largest Mesozoic deep marine unit originating in Ladinian; framed area—enlarged in c, BFZ Borovnica fault zone, ŽFZ Želimlje fault zone) (after Placer, 2008; Rožič, 2016). c Simplified geological map of the area with outcrops of Anisian platform carbonates (purple), Ladinian platform carbonates (yellow) and Ladinian basinal successions (green) marked (after Buser, 1968)–the framed area marks the location of the Kobilji curek basin (see Fig. 2 for details)

Back to article page