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
