Research news on neotectonic processes

Neotectonic processes are tectonic phenomena that have occurred from approximately the late Neogene to the present and are responsible for the current configuration and active deformation of the Earth’s crust. They include contemporary faulting, folding, crustal uplift and subsidence, active volcanism, and associated seismicity, typically constrained by geodetic measurements, seismic records, geomorphic analysis, and dating of displaced Quaternary deposits or landforms. Neotectonic processes are central to understanding present-day plate boundary kinematics, intraplate deformation, landscape evolution, and seismic and volcanic hazards, providing critical constraints on lithospheric rheology, stress fields, and the temporal variability of tectonic activity on human to Quaternary timescales.