Microstructural evidence for seismic and aseismic slip along clay-bearing, carbonate faults

In this multi-methodological study, microstructural 51 observations of fault rocks arecombined with micromechanical property analyses (Contact Resonance Atomic Force Microscopy, CR-AFM) and with rotary friction experiments (SHIVA apparatus) to find evidence of seismic to aseismic slip and understand the nanoscale rheology of clay-bearing, carbonate-hosted faults.
Fluidized structures, truncated clasts, pores and vesicles, and phyllosilicate nano-sized spherules and tubes suggest fast deformation events occurred during seismic slip, whereas clay-assisted pressure-solution processes, clumped clasts, foliation surfaces, and mantled clasts indicate slow deformation events occurred during postseismic/interseismic periods. CR-AFM measurements
show that the occurrence of ~5 wt.% of clay within the carbonate-hosted gouges can significantly reduce the fault core stiffness at nanoscale. In addition, during high-velocity friction experiments simulating seismic slip conditions, the presence of ultra-thin phyllosilicate-bearing (≤ 3 wt.%)
layers within calcite gouges, as those observed in the natural fault, show faster dynamic weakening than that of pure calcite gouges. The weak behavior of such layers could facilitate the upward propagation of seismic slip during earthquakes, thus possibly enhancing surface faulting.
Microstructural observations and experimental evidence fit some well-known geophysical and geodetic observations on the short- to long-term mechanical behavior of faults such as post67 seismic/interseismic aseismic creep, interseismic fault locking, and seismic slip propagation up to
the Earth’s surface.