Articles | Volume 17, issue 2
https://doi.org/10.5194/se-17-311-2026
https://doi.org/10.5194/se-17-311-2026
Research article
 | 
24 Feb 2026
Research article |  | 24 Feb 2026

The role of fault network geometry on the complexity of seismic cycles in the Apennines

Constanza Rodriguez Piceda, Zoë K. Mildon, Billy J. Andrews, Yifan Yin, Jean-Paul Ampuero, Martijn van den Ende, Claudia Sgambato, and Percy Galvez

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Cited articles

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Bagh, S., Chiaraluce, L., De Gori, P., Moretti, M., Govoni, A., Chiarabba, C., Di Bartolomeo, P., and Romanelli, M.: Background seismicity in the Central Apennines of Italy: The Abruzzo region case study, Tectonophysics, 444, 80–92, https://doi.org/10.1016/j.tecto.2007.08.009, 2007. 
Barbot, S.: Slow-slip, slow earthquakes, period-two cycles, full and partial ruptures, and deterministic chaos in a single asperity fault, Tectonophysics, 768, 228171, https://doi.org/10.1016/j.tecto.2019.228171, 2019. 
Bello, S., Lavecchia, G., Andrenacci, C., Ercoli, M., Cirillo, D., Carboni, F., Barchi, M. R., and Brozzetti, F.: Complex trans-ridge normal faults controlling large earthquakes, Sci. Rep., 12, 10676, https://doi.org/10.1038/s41598-022-14406-4, 2022. 
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Short summary
We investigate how the spatial arrangement of normal faults in the Italian Apennines affects earthquake timing and size. Computer-based models show that wide networks with faults offset across-strike produce more irregular and variable earthquakes, while narrow networks with fewer across-strike faults lead to more regular events. Faster-moving faults are more sensitive to nearby positive stress interactions, highlighting the need to consider fault geometry in seismic hazard assessments.
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