The Pannonian basin is an integral part of the convergence zone between the Eurasian and
Nubian plates characterized by active subductions of oceanic and continental plates, and …

The complex geodynamic history of the Paratethys periodically fostered the evolution of a
highly endemic biota with only limited exchange between the neighboring Mediterranean …

The architecture of sedimentary basins reflects the relationship between accommodation
space and sediment supply, their rates and localization being variable during basin …

A map-view palinspastic restoration of tectonic units in the Alps, Carpathians and Dinarides
reveals the plate tectonic configuration before the onset of Miocene to recent deformations …

The large number and distribution of rollback systems in Mediterranean orogens infer the
possibility of interacting extensional back‐arc deformation driven by different slabs. The …

The Miocene Central Paratethys Sea covered wide areas of the Pannonian Basin System,
bordered by the mountain chains of the Alps, Carpathians and Dinarides. The epicontinental …

Abstract Development of the rift-type North Croatian Basin located in the south-western
Neogene Pannonian Basin System and belonging to the Central Paratethys realm, was …

The Sava Zone of the northern Dinarides is part of the Cenozoic Adria‐Europe plate
boundary. Here Late Cretaceous subduction of remnants of Meliata‐Vardar oceanic …

In the Late Miocene–Early Pliocene Lake Pannon, regression went on for about 6Ma.
Sediments arriving from the Alpine–Carpathian source area were partly accumulated on the …

Sažetak The Pannonian Basin System (PBS) originated during the Early Miocene as a result
of extensional processes between the Alpine-Carpathian and the Dinaride Orogenic Belts …