The High Karst Unit of the External Dinarides is a tectonic unit established by French geologists, so-called Aubouin's group, as reviewed in a recent scientific literature.[3] The unit consists of a highly tectonically deformed carbonate and clastic rock successions deposited between the
Upper Carboniferous age of the
Carboniferous period in the
Mesozoic Era, and the
Eocene epoch of the
Paleogene period in the
Cenozoic Era.[4][5]
^Korbar, Tvrtko (2009). "Orogenic evolution of the External Dinarides in the NE Adriatic region: A model constrained by tectonostratigraphy of Upper Cretaceous to Paleogene carbonates". Earth-Science Reviews. 96 (4): 296–312.
Bibcode:
2009ESRv...96..296K.
doi:
10.1016/j.earscirev.2009.07.004.
^Vlahović, Igor; Tišljar, Josip; Velić, Ivo; Matičec, Dubravko (2005). "Evolution of the Adriatic Carbonate Platform: Palaeogeography, main events and depositional dynamics". Palaeogeography, Palaeoclimatology, Palaeoecology. 220 (3–4): 333–360.
Bibcode:
2005PPP...220..333V.
doi:
10.1016/j.palaeo.2005.01.011.
^Lóczy, Dénes; Stankoviansky, Miloš; Kotarba, Adam (2012). Recent landform evolution : the Carpatho-Balkan-Dinaric region. Dordrecht: Springer.
ISBN978-9400724471.