An upper limit for slow-earthquake zones: self-oscillatory behavior through the Hopf bifurcation mechanism from a spring-block model under lubricated surfaces
Related subject area
Subject: Bifurcation, dynamical systems, chaos, phase transition, nonlinear waves, pattern formation | Topic: Solid earth, continental surface, biogeochemistryExperimental study of forced convection heat transport in porous mediaComplex interplay between stress perturbations and viscoelastic relaxation in a two-asperity fault modelMultistable slip of a one-degree-of-freedom spring-slider model in the presence of thermal-pressurized slip-weakening friction and viscosityConditions for the occurrence of seismic sequences in a fault systemStress states and moment rates of a two-asperity fault in the presence of viscoelastic relaxation
Nonlin. Processes Geophys., 25, 279–290,2018
Nonlin. Processes Geophys., 25, 251–265,2018
Nonlin. Processes Geophys., 24, 467–480,2017
Nonlin. Processes Geophys., 23, 419–433,2016
Nonlin. Processes Geophys., 22, 349–359,2015
Abe, Y. and Kato, N.: Complex Earthquake Cycle Simulations Using a Two-Degree-of-Freedom Spring-Block Model with a Rate-and State-Friction Law, Pure Appl. Geophys., 170, 745–765, 2013.
Abe, Y. and Kato, N.: Intermittency of earthquake cycles in a model of a three-degree-of-freedom spring-block system, Nonlin. Processes Geophys., 21, 841–853, https://doi.org/10.5194/npg-21-841-2014, 2014.
Alvarez-Ramírez, J., Garrido, R., and Femat, R.: Control of systems with friction, Phys. Rev. E, 51, 6235, https://doi.org/10.1103/PhysRevE.51.6235, 1995.
Amendola, A. and Dragoni, M.: Dynamics of a two-fault system with viscoelastic coupling, Nonlin. Processes Geophys., 20, 1-10, https://doi.org/10.5194/npg-20-1-2013, 2013.
Andersson, S., Söderberg, A., and Björklund, S.: Friction models for sliding dry, boundary and mixed lubricated contacts, Tribol. Int., 40, 580–587, 2007.