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 …

Abstract The Pannonian Basin complex has approximately 13 billion BOE cumulative
production to date. As to the remaining resources, various estimates place the combined …

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

The past decade has witnessed spectacular progress in the collection of observational data
and their interpretation in the Pannonian Basin and the surrounding Alpine, Carpathian and …

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 …

Scaled sandbox models were used to investigate the 4D evolution of pull-apart basins
formed above underlap** releasing stepovers in both pure strike-slip and transtensional …

The data on the Neogene geodynamics, palaeogeography, and basin evolution of the
Western Carpathians, Northern Pannonian domain and adjoining areas (ALCAPA Mega …

This paper presents a latest compilation of data on the present-day stress pattern in the
Pannonian basin, and its tectonic environment, the Alpine–Dinaric orogens. Extensional …

The Mid-Hungarian line is a major tectonic feature of the Intra-Carpathian area separating
two terranes of different origin and tectonic structure. Although this tectonic line was known …

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 …