The stress recovery following an earthquake, on a fault where the initial strength threshold is preserved, is here considered in a “half-space” model. In this model a cracked horizontal elastic layer (the seismogenic crust) is welded to a viscoelastic, half-space substratum with Maxwell rheology (the ductile crust). The earthquake is modeled as a stress drop event ( crack) while in previous similar papers it was usually modeled as a “constant slip event”. Unlike crack models, constant slip dislocations are not suitable for describing the stress field in the proximity of the fault, particularly on the fault plane, which is the main concern of the present work. The fault becomes welded or “locked” immediately after the earthquake and can temporarily sustain the stress reloaded on it following the stress relaxation of the underlying ductile layer. Subsequent events are expected to be generated near the fault plane, at the location where the seismic stress drop is completely recovered by the postseismic reloading. Solutions show that, if the fault cuts most of the elastic upper layer, major aftershocks, or secondary earthquakes related to the first event, can occur in the deep section of the fault, within times comparable with the relaxation time of the ductile crust beneath the continents.