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

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Fig. 33 — a Illustration of virtual ruptures for earthquake of different magnitudes for a single point source; b virtual ruptures generated within a

source zone, which in practice could also have different orientations, dips and depths (Monelli et al. 2014)