The introduction of the linear slip-weakening friction law permits the solution of the elastodynamic equation for a rupture that develops on a fault by removing the singularity in the components of stress tensor, thereby ensuring a finite energy flux at the crack tip. With this governing model, largely used by seismologists, it is possible to simulate a single earthquake event; but, in the absence of remote tectonic loading, it requires the introduction of an artificial procedure to initiate the rupture (i.e., to reach the failure stress point). In this article, by studying the dynamic rupture propagation and the solutions on the fault and on the free surface, I systematically compare three conceptually and algorithmically different nucleation strategies widely adopted in the literature: the imposition of an initially constant rupture speed, the introduction of a shear stress asperity, and the perturbation to the initial particle velocity field. My results show that, contrary to supershear ruptures, which tend to forget their origins, subshear ruptures are quite sensitive to the adopted nucleation procedure, which can bias the runaway rupture. I confirm that the most gradual transition from imposed nucleation and spontaneous propagation is obtained by initially forcing the rupture to expand at a properly chosen, constant speed (0.75 times the Rayleigh speed). I also numerically demonstrate that a valid alternative to this strategy is an appropriately smoothed, elliptical shear stress asperity. Moreover, I evaluate the optimal size of the nucleation patch where the procedure is applied; the simulations indicate that its size has to equal the critical distance of Day (1982) in the case of supershear ruptures and to exceed it in the case of subshear ruptures.

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