Contrasting along-strike deformation styles in the central external Dinarides assessed by balanced cross-sections: Implications for the tectonic evolution of its …

P Balling, B Tomljenović, SM Schmid… - Global and planetary …, 2021 - Elsevier
The Cenozoic foreland fold and thrust belt of the external Dinarides along the eastern shore
of the Adriatic Sea shows an overall NW-SE structural strike that changes to EW in its central …

Discrimination of Rock Units in Karst Terrains Using Sentinel-2A Imagery

N Gizdavec, M Gašparović, S Miko, B Lužar-Oberiter… - Remote sensing, 2022 - mdpi.com
We explored the potential incorporation of Sentinel-2A imagery for rock unit determination in
the Croatian karst region dominated by carbonate rocks. The various lithological units are …

A time-space window between Eocene karst bauxite genesis and the first molasse deposition in the Dinaric Foreland Basin in the North Dalmatia, Croatia

V Brčić, I Dunkl, A Mindszenty, M Brlek… - Frontiers in Earth …, 2023 - frontiersin.org
Karst bauxite deposits in the North Dalmatian piggyback basin (NDPGB) are a part of the
Mediterranean bauxite belt, which is the largest European bauxite deposit zone; however …

Laterally variable development of a basin-wide transgressive unit of the North Dalmatian foreland basin (Eocene, Dinarides, Croatia)

L Babić, J Zupanič - Geologia Croatica, 2012 - hrcak.srce.hr
Sažetak The Palaeogene Promina Beds (PB), exposed in the Dinaric coastal range, is about
a 2km thick heterogeneous succession representing a late sedimentary fill of the North …

Sedimentary evolution of an inner foreland basin margin: Paleogene Promina Beds of the type area, Mt. Promina (Dinarides, Croatia)

J Zupanič, L Babić - Geologia Croatica, 2011 - hrcak.srce.hr
Sažetak Mt. Promina became famous for its coal mines, vertebrate remains and fossil flora,
and for the use of its name in denoting sediments covering a wide area of the Dinaric coastal …

Nearshore deposits in the middle Eocene clastic succession in northern Dalmatia (Dinarides, Croatia)

L Babić, J Zupanić - Geologia Croatica, 1998 - hrcak.srce.hr
Sažetak The Middle Eocene clastic succession in the Radovin Syncline is approximately
900 m thick and consists of hemipelagic and flysch-type deposits in its lower part, and …