Strain localization in sandstone-derived fault gouges under conditions relevant to earthquake nucleation

Constraining strain localization and the growth of shear fabrics within
brittle fault zones at sub-seismic slip rates are important for
understanding fault strength and frictional stability. We conducted direct
shear experiments on simulated sandstone-derived fault gouges at an
effective normal stress of 40 MPa, pore fluid pressure of 15 MPa, and
temperature of 100°C. Using a passive strain marker and X-ray Computed
Tomography (XCT), we analyzed the spatial deformation of the gouge samples
obtained from the strain-hardening stage to strain-softening stage to
steady-state at shearing velocities of 1, 30, and 1000 µm/s. We developed
a machine-learning-based automatic boundary detection method to recognize
the shear zone fabrics and quantify the slip partitioning between each
fabric element. Our results show that R1 and Y (or boundary) shears are
the two major shear zone fabrics. At velocities of 1 and 30 µm/s, the
relative amount of slip on R1 shears is displacement dependent and
increases to ~20% at the strain-softening stage and then decreases to
~10–18% at steady-state. This trend is absent at high velocity with an
amount of ~18% through all investigated stages. At all velocities, the
relative amount of slip on Y and boundary shears increases linearly with
displacement to a total of more than 50% at steady-state. Our study
provides constraints for the development of the active slip zone, which is
an important input parameter for the heat budget for small-magnitude
earthquakes with limited slip (mm-dm), such as those occurring in induced
seismicity.