Fig. 7From: Dynamic nucleation as a cascade-up of earthquakes depending on rupture propagation velocityEffect of spatial smoothing on \({D}_{C}\). A moving average of \(L={2}^{n}+1 (n=0, \dots , 6)\) is employed, and the results are presented for the anti-plane case. a Estimation of \({R}_{C}^{dyn}\). b Estimaton of \({\gamma }_{c}\). Note that \({v}_{i}\) is invariant, whereas \({D}_{C}\) increases linearly in the nucleation zoneBack to article page