Γ-convergence for a Fault Model with Slip-weakening Friction and Periodic Barriers
نویسندگان
چکیده
We consider a three-dimensional elastic body with a plane fault under a slip-weakening friction. The fault has -periodically distributed holes, called (smallscale) barriers. This problem arises in the modeling of the earthquake nucleation on a large-scale fault. In each -square of the -lattice on the fault plane, the friction contact is considered outside an open set T (small-scale barrier) of size r < , compactly inclosed in the -square. The solution of each -problem is found as local minima for an energy with both bulk and surface terms. The first eigenvalue of a symmetric and compact operator K provides information about the stability of the solution. Using Γ-convergence techniques, we study the asymptotic behavior as tends to 0 for the friction contact problem. Depending on the values of c =: lim →0 r / 2 we obtain different limit problems. The asymptotic analysis for the associated spectral problem is performed using Gconvergence for the sequence of operators K . The limits of the eigenvalue sequences and the associated eigenvectors are eigenvalues and respectively eigenvectors of a limit operator. From the physical point of view our result can be interpreted as follows: i) if the barriers are too large (i.e. c = ∞), then the fault is locked (no slip), Received March 11, 2005. 2000 Mathematics Subject Classification. Primary 35J25, 74Q05; Secondary 35P99, 74B10.
منابع مشابه
A constitutive model for fault gouge deformation in dynamic rupture simulations
In the context of numerical simulations of elastodynamic ruptures, we compare friction laws, including the linear slip-weakening (SW) law, the Dieterich-Ruina (DR) law, and the Free Volume (FV) law. The FV law is based on microscopic physics, incorporating Shear Transformation Zone (STZ) Theory which describes local, non-affine rearrangements within the granular fault gouge. A dynamic state var...
متن کاملUnlocking the effects of friction on fault damage zones
Two-dimensional, numerical models of a linear fault embedded within a linear elastic medium show the generation of off-fault tensile failure that results from inelastic slip along the fault. We explore quasistatic models with slip-weakening friction to assess the effects of spatially and temporally variable friction on the damage patterns. Tensile fractures form where tangential normal stresses...
متن کاملSensitivity of 3d Rupture Dynamics to Fault Geometry and Friction Parameters the Friction Law
We scale the various parameters deening a 3D fault model (i.e. characteristic distance and time of a state friction law, size and aspect ratio of the fault, medium impedance) and derive two dimensionless parameters governing the typical dynamics of the fault through single or multiple ruptures. The diier-ent faulting regimes are illustrated by a series of numerical simulations. As the parameter...
متن کاملScaling of small repeating earthquakes explained by interaction of seismic and aseismic slip in a rate and state fault model
[1] Because of short recurrence times and known locations, small repeating earthquakes present a rare predictable opportunity for detailed field observations. They are used to study fault creeping velocities, earthquake nucleation, stress drops, and other aspects of tectonophysics, earthquake mechanics, and seismology. An intriguing observation about repeating earthquakes is their scaling of re...
متن کاملFrictional weakening and slip complexity in earthquake faults
Previous work has shown that velocity-weakening friction produces slip complexity in simple dynamical models of earthquake faults ( Carlson and Langer, 1989). Rere I show that a different type of dynamical instability, caused by slipweakening friction, also produces slip complexity. The deterministically chaotic slip complexity produced by slip-weakening friction in a simple one dimensional mod...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
عنوان ژورنال:
دوره شماره
صفحات -
تاریخ انتشار 2005