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.

Seismic attenuation techniques reveal what lies beneath Taiwan

As seismic waves travel through Earth, they gradually lose energy, a process called attenuation. That energy loss doesn't happen uniformly—some features in the crust sap far more energy from seismic waves than others. Researchers ...

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