The Role of Fault Rock Fabric in the Dynamics of Laboratory Faults

Fault stability is inherently linked to the frictional and healing properties of fault rocks and associated fabrics. Their complex interaction controls how the stored elastic energy is dissipated, that is, through creep or seismic motion. In this work, we focus on the relevance of fault fabrics in controlling the reactivation and slip behavior of dolomite‐anhydrite analog faults. We designed a set of laboratory experiments where we first develop fault rocks characterized by different grain size reduction and localization at normal stresses of σN = 15, 35, 60, and 100 MPa and second, we reload and reactivate these fault rocks at the frictional stability transition, achieved at σN = 35 MPa by reducing the machine stiffness. If normal stress is lowered this way, reactivation occurs with relatively large stress drops and large peak‐slip velocities. Subsequent unstable behavior produces slow stick‐slip events with low stress drop and with either asymmetric or Gaussian slip velocity function depending on the inherited fault fabric. If normal stress is raised, deformation is accommodated within angular cataclasites promoting stable slip. The integration of microstructural data (showing brittle reworking of preexisting textures) with mechanical data (documenting restrengthening and dilation upon reactivation) suggests that frictional and chemically assisted healing, which is common in natural faults during the interseismic phase, can be a relevant process in developing large instabilities. We also conclude that fault rock heterogeneity (fault fabric) modulates the slip velocity function and thus the dynamics of repeating stick‐slip cycles. Plain Language Summary Displacement is accommodated within the Earth's upper crust through motion along fault zones. These fault zones are composed of a wide variety of deformed rocks, which are characterized by different geometric (e.g., inner textures) and physico‐chemical properties. Such complexity is key in controlling how the elastic energy stored in the loading medium surrounding the fault will be dissipated in time, for example, through slow (aseismic creep) or fast slip (earthquakes). This study presents a series of laboratory experiments where: (a) a range of pressures are applied to form fault rocks characterized by different inner textures; and then (b) the fault rocks are reactivated at the same experimental conditions, chosen to favor unstable sliding as documented in previous experiments in the same material. The