Effect of glass on the frictional behavior of basalts at seismic slip rates

We performed 31 friction experiments on glassy basalts (GB) and glass-free basalts (GFB) at slip rates up to 6.5m s(-1) and normal stress up to 40MPa (seismic conditions). Frictional weakening was associated to bulk frictional melting and lubrication. The weakening distance (D-w) was about 3 times shorter in GB than in GFB, but the steady state friction was systematically higher in GB than in GFB. The shorter D-w in GB may be explained by the thermal softening occurring at the glass transition temperature (T-g similar to 500 degrees C), which is lower than the bulk melting temperature (T-m similar to 1250 degrees C) of GFB. Postexperiment microanalyses suggest that the larger crystal fraction measured in GB melts results in the higher steady state friction value compared to the GFB melts. The effect of interstitial glass is to facilitate frictional instability and rupture propagation in GB with respect to GFB. Key Points First experiments on basalts at seismic slip rates Interstitial glass renders the basalts more prone to frictional instabilities Interstitial glass in basalts increases the steady-state friction