Micro-slips inside a granular shear band as nano-earthquakes

TL;DR

This study experimentally investigates micro-slips within a granular shear band, revealing that their statistical and causal properties mirror natural earthquakes, thus providing insights into earthquake physics at the laboratory scale.

Contribution

First laboratory demonstration of causal and statistical earthquake-like micro-slip dynamics in a granular shear band using seismology-inspired analysis methods.

Findings

Micro-slips follow empirical earthquake laws

Spatio-temporal correlations emerge from triggering kernels

Strain, not time, controls memory effects

Abstract

We study experimentally the fluctuations of deformation along a shear fault naturally emerging within a compressed frictional granular medium. Using laser interferometry, we show that the deformation inside this granular gouge occurs as a succession of localized micro-slips distributed along the fault. The associated distributions of released seismic moments, the memory effects in strain fluctuations, as well as the time correlations between successive events, follow exactly the empirical laws of natural earthquakes. Using a methodology initially developed in seismology and social science, we reveal, for the first time at the laboratory scale, the underlying causal structure. This demonstrates that the spatio-temporal correlations of the slip dynamics effectively emerge from more fundamental triggering kernels. This formal analogy between natural faults and our experimentally controllable granular shear band opens the way towards a better understanding of earthquake physics. In particular, comparing experiments performed under different imposed deformation rates, we show that strain, not time, is the right parameter controlling the memory effects in the dynamics of our fault analog. This raises the fundamental question of the relative roles of strain-dependent structural rearrangements within the fault gouge vs that of truly time-dependent, thermally activated processes, in the emergence of spatio-temporal correlations of natural seismicity.