The cumulative incision rates of~ 50–70 m/Ma integrating over the last~ 3 Ma have been
derived from published terrace-chronological data of the Danube river in the Western …

This study aims at a new quantification of neotectonic deformation of the central part of the
Pannonian Basin. We use terrace levels and associated travertine as well as speleothem …

Subsidence, sedimentation and tectonic quiescence of the Pannonian basin was interrupted
a few million years ago by tectonic reactivation. This recent activity has manifested itself in …

Most of the recent geodynamic interpretations of the Pannonian Basin focus on its relation to
the formation of the Carpathians and the Alpine orogeny. However, also the Dinarides were …

The Transdanubian Range (TR) suffered a moderate extension during the rifting of the
Pannonian basin between~ 18 and~ 11 Ma. Post-rift phase was connected to the deposition …

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 development of the northern Danube Basin (nDB) was closely related to the Late
Miocene geodynamic evolution of the Pannonian Basin System. It started with a wide rifting …

The Someș fluvial fan is located in the NW extremity of the Great Hungarian Plain
(Pannonian Basin). It was formed by the left-side tributaries of the Tisa River (a tributary of …

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 …

We present a comprehensive review on what we have learned during the last decade and
what we need to know in the future about the present-day crustal deformation and …