Abstract
We significantly improved a numerical seismo-thermo-mechanical model to - besides long-term subduction dynamics - also accurately simulate the dynamics of short-term seismogenesis. Through adaptive time stepping and rate-and-state friction we can resolve events from aseismic to coseismic slip, including wave propagation. Through High-Performance-Computing and non-linear solvers we can accurately do this in 3D. Results showing grid size convergence demonstrate the existence of a fault parallel length scale on the order of (tens of) meters for slow slip transients.
Original language | English |
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Pages | 1037-1038 |
Number of pages | 2 |
Publication status | Published - 1 Jan 2017 |
Event | 14th International Conference on Fracture, ICF 2017 - Rhodes, Greece Duration: 18 Jun 2017 → 20 Jun 2017 |
Conference
Conference | 14th International Conference on Fracture, ICF 2017 |
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Country/Territory | Greece |
City | Rhodes |
Period | 18/06/17 → 20/06/17 |