New PhDONE – Congrats Michela!

New PhDONE – Congrats Michela!

09/02/2026 Perigeo 0
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On January 15, 2026 Michela Colombo successfully defended her PhD thesis entitled “Uncertainty in Probabilistic Fault Displacement Hazard Analysis: a sensitivity study and application to the Rieti Basin (Central Italy)”.

Michela’s project was realized in the framework of the Geosciences-IR project, coordinated by Ispra and devoted to the development of a cloud research infrastructure, useful for the regional Geological surveys of Italy.

Michela’s thesis explores three main aspects:

  • Sensitivity analysis to evaluate the influence of the several parameters that are used as input data for fault displacement hazard assessment in a probabilistic framework (PFDHA). This was carried out by applying a “one factor at a time” method.
  • Application of the PFDHA approach to a case study, building upon the work recently published by our group (Livio et al., 2026) that involved extensive paleoseismic trenching in the Rieti basin.
  • Update of the SURE (Surface Rupture due to Earthquakes) database, which represent a standardized compilation of rupture maps and fault displacement measurements.

The results have both a theoretical and applied valency, pointing to the need to carefully evaluate the source of uncertainty in PFDHA studies. Indeed, each input parameter has a peculiar impact on the obtained hazard curve (Figure 1).

Figure 1: Example of a tornado plot, ranking the influence of the input parameters for strike-slip earthquakes. The annual frequency of exceedance is sampled at two reference displacement values, namely 10 cm and 2 m.

The application of the methodology to the Rieti basin provides a preliminary estimate of fault displacement hazard (Figure 2) and paves the road for more detailed studies in the same area and in other similar regions.

Figure 2: hazard curve for distributed ruptures, referred to the Eastern Segment of the fault bordering the southern part of the Rieti basin. Curves are calculated for three distinct distances from the principal fault traces (100 m, 200 m, and 500 m), for both the hanging wall (solid lines) and the footwall (dashed lines). Dashed horizontal lines indicate different exceedance probabilities (1%, 2%, and 10%) over a 200-year interval.

Congratulations Michela!

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