Extension and associated tectonic exhumation have been described across a diverse
spectrum of geodynamic environments, ranging from lithospheric-scale extension along …

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 …

" Department of Geophysics, Eötvös University, Budapest, 1085 Ludovika tér 2. Hungary
“Department of Engineering Geology, Technical University of Budapest, Stoczek u. 2 …

Hungary lies in the central part of the Pannonian Basin, surrounded by the ranges of the
Alps, Carpathians, and Dinarides. The geology of the country can be summarized as a …

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

Abstract in English The Miocene Central Paratethys Sea covered wide areas of the
Pannonian Basin System, bordered by the mountain chains of the Alps, Carpathians and …

The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene
extension exerting a profound effect on the lithospheric configuration, which continues even …

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 post-flysch (Oligocene–Miocene) palaeogeographic evolution of the entire North Alpine
Foreland Basin (NAFB) between Savoy (France) and Lower Austria is presented in eight …