Preprints
https://doi.org/10.5194/egusphere-2025-4886
https://doi.org/10.5194/egusphere-2025-4886
24 Nov 2025
 | 24 Nov 2025
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

A fault-based application to model seismicity rates for seismic hazard assessment in the southern Apennines (Italy)

Giulia Alessandrini, Octavi Gómez-Novell, Silvia Castellaro, Michela Giustiniani, and Umberta Tinivella

Abstract. Although fault-based approaches to seismic hazard assessment have been increasingly adopted worldwide, the official Italian hazard model, on which the national building code is based, still relies on a catalogue-based framework, with well-known limitations in capturing the long-term recurrences of large-magnitude events. In this study, we present a fault-based application to model seismicity rates for the southern Apennines (Italy) that incorporates a multi-fault rupture assumption. This area is of particular interest due to its active seismicity and the presence of large dams, for which robust long-term hazard estimates are essential. We use the SHERIFS code to model seismicity rates at the fault system-level, which allow us to explore epistemic uncertainties of fault and seismicity parameters (rupture scenarios, scaling laws, b-values and background seismicity). Our results highlight the key role of rupture models: scenarios allowing multi-fault ruptures outperform single-fault rupture models in terms of agreement with the regional seismicity and paleoseismic rates. Our findings support the inclusion of multi-fault rupture models in PSHA logic trees for the region and emphasize the need for improved fault behaviour characterization in southern Italy.

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Giulia Alessandrini, Octavi Gómez-Novell, Silvia Castellaro, Michela Giustiniani, and Umberta Tinivella

Status: open (until 06 Jan 2026)

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Giulia Alessandrini, Octavi Gómez-Novell, Silvia Castellaro, Michela Giustiniani, and Umberta Tinivella

Data sets

Dataset for fault-based seismicity rates in the southern Apennines (Italy) G. Alessandrini et al. https://doi.org/10.5281/zenodo.17183318

Giulia Alessandrini, Octavi Gómez-Novell, Silvia Castellaro, Michela Giustiniani, and Umberta Tinivella

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Short summary
We model fault-based seismicity rates (expected number of earthquakes over time): instead of relying on past earthquake records, we calculate these rates by converting the slip rates of active faults into earthquake activity, both for individual faults and for ruptures involving several adjacent faults. Our results show that the latter better match observations and past geological evidence, and highlight the importance of incorporating complex fault interactions into seismic hazard models.
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