| Studying Active Faults from the Near-Surface to Seismogenic Depth: From Multiscale Observations to Integrated Tectonic and Seismotectonic Models
TS3
Studying Active Faults from the Near-Surface to Seismogenic Depth: From Multiscale Observations to Integrated Tectonic and Seismotectonic Models
Co-organized by GD/NH4/SM, co-sponsored by ILP
Convener: Vanja Kastelic | Co-conveners: Fabio Luca Bonali, Marco Bohnhoff, Federica Ferrarini, Cristina Totaro

Active fault systems record deformation across a wide range of spatial, temporal, and depth scales, from fault exposures and surface landforms to crustal structures, earthquake processes, and regional tectonic frameworks. Connecting these different scales is central to understanding how faults develop, interact, and accommodate deformation, and to building robust tectonic and seismotectonic models of active regions. Now in its fifth edition, this session provides an inclusive forum for the active-tectonics and seismotectonics community to present new observations, methodological developments and interpretations that advance our understanding of fault-system geometry, kinematics, evolution and seismogenic behaviour.
We welcome contributions ranging from detailed studies of individual faults and earthquake sequences to meso- and regional-scale investigations, across different tectonic regimes and geological settings, including volcanic and submarine environments. Field observations, structural geology, neotectonics, paleoseismology, tectonic geomorphology, remote sensing, geodesy, geophysics and seismology all provide complementary constraints on fault geometry and segmentation, slip rates, stress and strain fields, crustal deformation, fault interaction and tectonic evolution. Single-method studies, comparisons among techniques and multidisciplinary investigations are equally encouraged. The session welcomes contributions from researchers at all career stages, with particular encouragement to early-career scientists.
Particular interest is placed on studies that strengthen links between surface observations and fault geometry at seismogenic depth, connect deformation across different timescales, or place local fault behaviour within broader tectonic and seismotectonic frameworks. Numerical, analytical and analogue modelling, together with innovative computational approaches such as artificial intelligence and machine learning, are also welcome where they support the analysis, integration or interpretation of active-tectonic and seismotectonic information.
By bringing together diverse observations, methods and scales, the session aims to stimulate exchange across disciplines and advance transferable, testable models of active fault systems, their evolution and their relationship with earthquake occurrence and seismic hazard.