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 Gödöllő Hills, a low-relief terrain within the Central Pannonian Basin in Hungary, is
characterised by moderate tectonic deformation rates. Although typical tectonic landforms …

During the last two decades teleseismic studies yielded valuable information on the
structure of the upper mantle below the Alpine–Mediterranean area. Subducted oceanic …

During the last decade, a series of controlled source seismic experiments brought new
insight into the crustal and lithospheric structure of the Eastern Alps and their adjacent …

Alp01 and Alp02 are the longest profiles recorded during ALP 2002, a large international
seismic refraction and wide‐angle reflection experiment undertaken in the Eastern Alps in …

Subducted slab roll-back, lithospheric instability and asthenospheric extrusion have all been
proposed as mechanisms that explain the evolution of the extensional Pannonian Basin …

We provide a present-day surface-kinematics model for the Alpine region and surroundings
based on a high-level data analysis of about 300 geodetic stations continuously operating …

We present an integrated gravity model of the European lithosphere based on an analysis of
a number of new data-sets, leading to a much higher resolution than provided by previous …

Abstract The Neogene to Quaternary lateral extrusion of the Eastern Alps towards the
Pannonian Basin is accommodated by a system of strike-slip faults. Despite decades-lasting …

The Vienna Basin at the transition between the Alpine and Carpathian belt hosts a number
of large Pleistocene sub‐basins forming along an active continental scale strike‐slip fault …