Which outcome occurs when repeating moderate shear stress oscillations along tectonic faults reaching a critical instability threshold?

💡 Explanation

Aseismic creep accelerates because transient stress changes induce rate-and-state friction via elastic deformation along faults, encouraging slow slip rather than abrupt rupture. Therefore creep accelerates, rather than triggering seismic events or altering geological processes substantially due to slow movements.

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