Frictional restrengthening in simulated fault gouge: Effect of shear load perturbations

被引:61
作者
Karner, SL [1 ]
Marone, C [1 ]
机构
[1] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
关键词
D O I
10.1029/2001JB000263
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Laboratory friction experiments are important for understanding fault restrengthening (healing) between failure events. To date, studies have focused mainly on time and velocity dependence of friction for small perturbations about conditions for steady state sliding. To investigate healing under a wider range of conditions, as appropriate for the interseismic period and dynamic rupture on seismogenic faults, we vary shear load for holds tau (hold), hold time t(h), load point velocity V, and initial gouge layer thickness T-0. We shear layers of granular quartz in a biaxial testing apparatus at room temperature and humidity. In addition to conventional slide-hold-slide (CSHS) healing tests, we perform tests in which shear stress is rapidly reduced prior to each hold. Identical slip histories are used in all experiments. Our CSHS tests show time-dependent healing, where Delta mu is the difference between peak static friction and prehold sliding friction, consistent with previous work. For a given t(h) we find a systematic increase in peak static strength and Delta mu with decreasing tau (hold) (for t(h) = 100 s, Delta mu = 0.007 for CSHS tests and 0.05 for tau (hold) = 0 tests). Significantly, healing tests at zero shear stress show decreasing static frictional yield strength with increasing t(h); thus we observe time-dependent weakening in this case. We vary initial layer thickness (0.5-3 mm) and find greater healing for thicker layers. Numerical simulations using rate and state friction laws show that neither the Dieterich nor Ruina evolution laws predict our experimentally observed healing rates for the full range of conditions studied. Our results have significant implications for the mechanics of deformation within granular media. We present a micromechanical model based on stress chains, jamming, and time-dependent unjamming of sheared granular layers. As applied to earthquakes, our data indicate that coseismic stress drop is expected to have an important effect on fault healing rates and static yield strength.
引用
收藏
页码:19319 / 19337
页数:19
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