The present paper introduces the new 1:500 000 scale map of young geological deformations in Hungary, including all important deformation structures (faults and folds) related to the neotectonic evolutionary phase (<6–8 Ma) of the Pannonian basin. The new map is based on the interpretation of nearly 2900 2D seismic profiles and 70 3D seismic volumes, as well as on the critical evaluation of the results of published neotectonic studies. An important novelty of the map is that not only the near-surface manifestations of the neotectonic faulting, but also their roots in the underlying pre-Pannonian substratum are displayed, allowing correlation between various reactivated fault segments of longer fault zones and aiding the better understand...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
The crustal structure of the transition zone between the Eastern Alps and the western part of the Pa...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
The new 1:500 000 scale map of young geological deformations in Hungary completed in 2020 based upon...
The new 1:500 000 scale map of young geological deformations in Hungary completed in 2020 based upon...
Hungary lies entirely within the Carpatho-Pannonian Region (CPR), a dominant tectonic unit of easter...
In the Pannonian Basin fault-slip analysis and palaeostress determinations started in 1982–1984 by t...
The mechanism of earthquake occurrence in the Pannonian Basin is not clear in most cases (in other w...
Strike-slip tectonics has been the dominant style of deformation during the neotectonic (Pliocene an...
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and struc...
The past decade has witnessed spectacular progress in the collection of observational data and their...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
The crustal structure of the transition zone between the Eastern Alps and the western part of the Pa...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by m...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
The new 1:500 000 scale map of young geological deformations in Hungary completed in 2020 based upon...
The new 1:500 000 scale map of young geological deformations in Hungary completed in 2020 based upon...
Hungary lies entirely within the Carpatho-Pannonian Region (CPR), a dominant tectonic unit of easter...
In the Pannonian Basin fault-slip analysis and palaeostress determinations started in 1982–1984 by t...
The mechanism of earthquake occurrence in the Pannonian Basin is not clear in most cases (in other w...
Strike-slip tectonics has been the dominant style of deformation during the neotectonic (Pliocene an...
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and struc...
The past decade has witnessed spectacular progress in the collection of observational data and their...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
Understanding the formation and evolution of sedimentary basins is of paramount importance because t...
The crustal structure of the transition zone between the Eastern Alps and the western part of the Pa...