Graphite is considered as a material that promotes fault weakening and electrical conductivity (σ) enhancement at fault zones. We studied how shear deformation may affect the evolution of friction and electrical conductivity of synthetic quartz (Qz)-graphite (Gr) mixtures and, more importantly, whether the σ of the mixtures present visible changes at the beginning of the simulated fault slip. Long-displacement friction experiments were performed on 1.2–2.3 mm-thick gouge specimens of varied Gr volume fraction (X_Gr = 0–100 vol.%) under identical normal stress (2 or 5 MPa), slip rate (~1.0 mm/s), and N₂-flushing conditions. The experimental results suggested that the σ of the specimens with ≥ 4.6 vol.% X_Gr abruptly increased under limited shear displacement. With continued shear, the steady-state electrical conductivity (σ_ss) increased by more than seven orders of magnitude when X_Gr > 3.4 vol.%, while the steady-state frictional coefficient remained high (0.54–0.80) except for the specimens with X_Gr > 13.6 vol.%. The post-mortem microstructures revealed that the high σ_ss observed in the intermediate Gr content specimens (3.4–13.6 vol.%) is associated with an ad-hoc fabric (graphite–cortex clasts) present in the principal slip zone. For high Gr content, excess Gr flakes fill the pores and help develop mechanically lubricated surfaces. We propose that low Gr content (i.e., as low as 3.4 vol.%) can cause high conductivity anomalies in natural shear zones. Overall, the findings suggest that the initiation of slips within carbonaceous shear zones can be detected by identifying unusual temporal signals using electromagnetic stations.