[HTML][HTML] Hydro-mechanical earthquake cycles in a poro-visco-elasto-plastic fluid-bearing fault structure
A major goal in earthquake physics is to derive a constitutive framework for fault slip that
captures the dependence of shear strength on fault rheology, sliding velocity, and pore-fluid …
captures the dependence of shear strength on fault rheology, sliding velocity, and pore-fluid …
Modeling megathrust earthquakes across scales: One‐way coupling from geodynamics and seismic cycles to dynamic rupture
Taking the full complexity of subduction zones into account is important for realistic modeling
and hazard assessment of subduction zone seismicity and associated tsunamis. Studying …
and hazard assessment of subduction zone seismicity and associated tsunamis. Studying …
Subduction earthquake sequences in a non-linear visco-elasto-plastic megathrust
We present a 2-D thermomechanical computational framework for simulating earthquake
sequences in a non-linear visco-elasto-plastic compressible medium. The method is …
sequences in a non-linear visco-elasto-plastic compressible medium. The method is …
Seismic and aseismic fault growth lead to different fault orientations
S Preuss, R Herrendörfer, T Gerya… - Journal of …, 2019 - Wiley Online Library
Orientations of natural fault systems are subject to large variations. They often contradict
classical Coulomb failure theory as they are misoriented relative to the regional …
classical Coulomb failure theory as they are misoriented relative to the regional …
A secondary zone of uplift due to megathrust earthquakes
Y van Dinther, LE Preiswerk, TV Gerya - Pure and Applied Geophysics, 2019 - Springer
Abstract The 1960 M9. 5 Valdivia and 1964 M9. 2 Alaska earthquakes caused a decimeters
high secondary zone of uplift a few hundred kilometers landward of the trench. We analyze …
high secondary zone of uplift a few hundred kilometers landward of the trench. We analyze …
[PDF][PDF] Modelling coupled subduction and earthquake
Studying seismicity requires numerical methods that span a large range of spatial 16 and
temporal scales. We present the first coupled framework that resolves subduction 17 …
temporal scales. We present the first coupled framework that resolves subduction 17 …