Geological Formations and Processes Exploration

The Carpathian-Pannonian region of central Europe records one of the most geometrically complex episodes of continental tectonics in the Cenozoic, where the collision of the African and European plates during the Alpine orogeny drove the simultaneous back-arc extension that opened the Pannonian Basin during the Miocene. Geophysicists study this area to reconstruct how the crust thinned and deformed, how subducting slabs influenced surface topography, and how seismic wave behavior reveals the layered structure of the lithosphere beneath the region today. A central challenge is reconciling the evidence from seismicity, gravity anomalies, and tomographic imaging into a coherent picture of how subduction rollback, crustal shortening in the Carpathian arc, and basin subsidence unfolded together over roughly ten million years. Active research continues to refine the timing and kinematics of these events, particularly the degree to which lower-crustal flow versus brittle faulting controlled deformation, and what drives the region's ongoing seismicity.

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Keywords

Carpathian-Pannonian regiontectonic evolutionAlpine orogenyPannonian BasingeodynamicNeogene