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February 21, 2026Procedia Structural Integrity0 citationsOpen Access

Issues in near-source probabilistic seismic hazard analysis of the Messina Strait (Italy): preliminary investigation

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IIIunio IervolinoGBGeorgios BaltzopoulosECEugenio Chioccarelli

Key Points

  • The aim is to examine near-source effects on seismic hazard analysis for the Messina Strait, particularly focusing on forward rupture directivity and earthquake occurrence models.
  • Conducted near-source probabilistic seismic hazard analysis for a coastal site
  • Considered impulsive ground motion effects due to forward rupture directivity
  • Evaluated two earthquake occurrence models: Brownian passage time and slip-predictable model
  • Spectral pseudo-acceleration increases over 50% for earthquakes of magnitude M7±0.3 in specific vibration periods
  • Absolute differences in spectral acceleration remain low, under 0.08g
  • BPT and SPM yield lower probabilities of an earthquake occurring within 200 years compared to the homogeneous Poisson process

Abstract

One challenge for construction projects of strategic importance near known faults, is incorporating near-source (NS) effects in probabilistic seismic hazard analysis (PSHA) to define design actions. The most prominent NS effect with engineering relevance is forward rupture directivity, which can cause ground velocity pulses to manifest at sites pseudo-aligned with the direction of rupture propagation, leading to peculiar spectral amplitudes and inelastic-to-elastic ratios. Another issue is mainshock occurrence process on specific faults, which may depart from the homogeneous Poisson process (HPP), typically assumed for large-scale seismic source zones. This work offers a preliminary examination of such NS issues for the Messina Strait, where the 1908 M7.1 earthquake occurred. First, a NS-PSHA – conditional to event occurrence on the fault – is performed for a coastal site, accounting for impulsive ground motion occurrence. Second, two alternative earthquake occurrence models, accounting for the seismic history of the source are considered, the Brownian passage time (BPT) and the slip-predictable model (SPM), calibrated against available information about the fault. It is found that due to pulse-like effects, the relative increase in spectral pseudo-acceleration caused by a magnitude M7±0.3 earthquake occurring on the fault exceeds 50% for vibration periods between 3s and 10s, yet this corresponds to absolute differences lower than 0.08g. Moreover, both BPT and SPM yield lower probabilities of at least one earthquake occurring within the next two-hundred years, compared to the corresponding result from HPP. These probabilities are respectively 0.060 and 0.134 for BPT and SPM, compared to 0.237 from HPP.

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Cite This Study

Iervolino et al. (2026) studied this question.

synapsesocial.com/papers/69994b01873532290d01f51bhttps://doi.org/10.1016/j.prostr.2025.12.198
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