The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

This review considers the magmatic processes in the Carpathian–Pannonian Region (CPR)
from Early Miocene to Recent times, as well as the contemporaneous magmatism at its …

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

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 …

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

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

The youngest regional chronostratigraphic unit of the Central Paratethys, the Pannonian
Stage, is benchmarked by the deposits of Lake Pannon, containing a highly endemic …

This research aims to explore the application of an unsupervised machine learning and
inverse modeling-based methods to map the aquifers geometry and investigate the …

Advances in sedimentology and basin analysis provide the foundation for a comprehensive
basin-fill model and lithostratigraphic framework of Lake Pannon, Central Europe …