GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 2.1 GNGTS 2024 Fig. 2: Coefficients of variation for seismicity along the most important seismogenic structures in New Zealand between 1985 and 2022. (A) Local coefficient of variation and maximum observed magnitudes from 1920 and 2022 above Mw 6.0. Large seismic events tend to occur where seismic activity is locally Poissonian. (B) Global coefficient of variation and maximum historical magnitudes from 1920 and 2022. Large seismic events tend to occur where seismicity is globally clustered.

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