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This is a Observational study (also classified as: In Vitro Study, Animal Study).

September 5, 2025Open Access

A Multidisciplinary Approach to Mapping Morphostructural Features and Their Relation to Seismic Processes

Key Points

The study identified a correlation between seismic activity and morphostructural features in southwestern Sicily.
Utilizing methods such as Horizontal-to-Vertical Spectral Ratio (HVSR) and Electrical Resistivity Tomography (ERT), we mapped ground vulnerability.
Fractures observed were analyzed to understand their links to tectonic processes and potential subsurface fluid contributions.
The integration of multitemporal satellite imagery and seismic event distribution aided in assessing the spatial evolution of these features.

Abstract

A multidisciplinary investigation was conducted in southwestern Sicily, near the seismically active Belice Valley, based on the analysis of morphostructural features. These were observed as open fractures between 2014 and 2017; they were subsequently filled anthropogenically and then reactivated during a seismic swarm in 2019. We generated a seismic event distribution map to analyze the location, magnitude, and depth of earthquakes. This analysis, combined with multitemporal satellite imagery, allowed us to investigate the spatial and temporal relationship between seismic activity and fracture evolution. To investigate the spatial variation in thickness of the superficial cover and to assess the depth to the underlying bedrock or stiffer substratum, 45 Horizontal-to-Vertical Spectral Ratio (HVSR) ambient noise measurements were conducted. This method, which analyzes the resonance frequency of the ground, produced maps of the amplitude, frequency, and vulnerability index of the ground (Kg). By inverting the HVSR curves, constrained by Multichannel Analysis of Surface Waves (MASW) results, a subsurface model was created aimed at supporting the structural interpretation by highlighting variations in sediment thickness potentially associated with fault-controlled subsidence or deformation zones. The surface investigation revealed depressed elliptical deformation zones, where mainly sands outcrop. Grain-size and morphoscopic analyses of sediment samples helped understand the processes generating these shapes and predict future surface deformation. These elliptical shapes recall the liquefaction process. To investigate the potential presence of subsurface fluids that could have contributed to this process, Electrical Resistivity Tomography (ERT) was performed. The combination of the maps revealed a correlation between seismic activity and surface deformation, and the fractures observed were interpreted as inherited tectonic and/or geomorphological structures.

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