T026
Integrating Plate Interface Rheology and Seismicity with Subduction Zone Geodynamics

Session ID#: 81197

Session Description:
The rheological and frictional properties of the plate interface determine the degree of interseismic locking, seismic rupture size and the geodynamic coupling that influences long-term crustal deformation and possibly plate velocities. In turn, the interface rheology is influenced by petrology, stress state, temperature, fluid pressure and sediment thickness, which are all controlled by the broader geodynamics. A holistic understanding requires integrated studies of spatial scales ranging from fault/shear zones to tectonic plates and temporal scales from seconds to million-years. We welcome contributions from all relevant disciplines that use observations or models to explore the relationships between fault/shear zone rheology, megathrust seismicity and broad-scale geodynamics.
Index Terms:

8123 Dynamics: seismotectonics [TECTONOPHYSICS]
8163 Rheology and friction of fault zones [TECTONOPHYSICS]
8170 Subduction zone processes [TECTONOPHYSICS]


Primary Convener:  Adam Beall, Cardiff University, School of Earth and Ocean Sciences, Cardiff, CF24, United Kingdom
Conveners:  Whitney M Behr, ETH Swiss Federal Institute of Technology Zurich, Department of Earth Sciences, Zurich, Switzerland, Luca Dal Zilio, California Institute of Technology, Pasadena, United States and YaJing Liu, McGill University, Earth and Planetary Sciences, Montreal, QC, Canada
Primary Liaison:  Adam Beall, Cardiff University, School of Earth and Ocean Sciences, Cardiff, CF24, United Kingdom
 
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