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. 2022 Apr 22;20(6):2825–3069. doi: 10.1007/s10518-022-01357-4

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Fig. 26 — Illustration of the effect of truncating the distribution of ground-motion residuals by imposing different values of $ε_{\max}$ in PSHA calculations for regions of low (upper) and high (lower) seismicity rates (Bommer et al. 2004)