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 Pannonian Basin is a continental back-arc basin. Palaeomagnetics defined three
terranes: Alcapa (Alps–Carapathians–Pannonian), Tisza–Dacia and Dinarides, rotated …

Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the
Alpine–Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza …

The formation of the North Croatian Basin, which represents the south‐western marginal
part of the Pannonian Basin System and the Central Paratethys Bioprovince, began during …

Abstract Analysis of Neogene–Quaternary structures from seismic lines, surface
measurements and geological-mapping is presented from the border zone between the …

This paper attempts to explain the tectonic history and possible reasons for the change of
trend of the northwestern part of the Internal Dinarides in a transitional area between the …

We carried out an integrated paleomagnetic and structural study in the Transdanubian
Range, western and central Hungary. As a result, the Tertiary tectonic history of this area can …

Over the last 65 Ma, our world assumed its modern shape. This timespan is divided into the
Palaeogene Period, lasting from 65 to 23 Ma and the Neogene, which extends up to the …

With the aim of obtaining Tertiary palaeomagnetic directions for the Adriatic Foreland of the
Dinaric nappe system, we carried out a palaeomagnetic study on platform carbonates from …

Sažetak In the North Croatian Basin which is located in the southwestern part of the
Pannonian Basin System, Miocene tuff deposits have been observed at several localities in …