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 …

We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …

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 …

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

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 …

Abstract The Tokaj Mts. volcanism occurred in a thinning continental lithosphere regime at
the final stage of the subduction process. Using high-precision zircon U-Pb dating, four …

The Vrancea region of the south-eastern Carpathians is a remarkable site of intra-
continental intermediate-depth seismicity. A large set of geological, geophysical, and …

Lithospheric folding is an important mode of basin formation in compressional intraplate
settings. Basins formed by lithospheric folding are characterized by distinct features in …

Terra Nova, 22, 155–165, 2010 Abstract Sequence stratigraphy in the hinterland, kinematic
analysis of thin‐skinned thrusting in the foreland and thermochronological tracking of …