Pages that link to "Item:Q2862274"
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The following pages link to A model of rupturing lithospheric faults with reoccurring earthquakes (Q2862274):
Displaying 12 items.
- On the relation between gradient flows and the large-deviation principle, with applications to Markov chains and diffusion (Q471066) (← links)
- Theory of fast tectonic waves (Q1097740) (← links)
- A fault model with two asperities of different areas and strengths (Q1789234) (← links)
- Seismic waves and earthquakes in a global monolithic model (Q1790127) (← links)
- A general thermodynamical model for adhesive frictional contacts between viscoelastic or poro-viscoelastic bodies at small strains (Q2327761) (← links)
- Geophysical models of heat and fluid flow in damageable poro-elastic continua (Q2359851) (← links)
- Existence results for a coupled viscoplastic-damage model in thermoviscoelasticity (Q2360467) (← links)
- Perfect plasticity with damage and healing at small strains, its modeling, analysis, and computer implementation (Q2790408) (← links)
- Analysis of a dislocation model for earthquakes (Q2821879) (← links)
- Quasistatic adhesive contact delaminating in mixed mode and its numerical treatment (Q2950712) (← links)
- Coupling Rate-Independent and Rate-Dependent Processes: Existence Results (Q5737794) (← links)
- A convective model for poro-elastodynamics with damage and fluid flow towards Earth lithosphere modelling (Q6049937) (← links)
