Temporal and spatial changes in seismic attenuation associated with inferred fluid migration in the 2016 central Apennines earthquake sequence

Bulletin of the Seismological Society of America
National Institute of Geophysics and Volcanology (INGV), UC Berkeley
By: , and 

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Abstract

Prior work suggests that high‐frequency seismic attenuation acts as a highly sensitive proxy for crustal permeability and fluid mobility in fractured media. We test the hypothesis that the fault system responsible for the 2016–2017 Amatrice–Visso–Norcia–Capitignano sequence acted as an impermeable seal, compartmentalizing pressurized fluids until dynamic rupture triggered widespread fluid diffusion. By tracking across the sequence the spatiotemporal evolution of the S‐wave anelastic attenuation parameter, we identify large, positive low‐frequency attenuation anomalies emerging within the hanging wall following the Amatrice mainshock and strictly preceding subsequent large ruptures. Conversely, we observe weaker, negative anomalies in the footwall, anticorrelated in time with those of the hanging wall, revealing a massive asymmetry in fluid redistribution and permeability evolution across the fault system. Furthermore, aftershock migration rates reveal distinct linear alignments in a distance‐reduced time space, allowing us to explicitly track and quantify episodes of lateral and upward fluid migration. These physically consistent patterns suggest that stress‐driven fluid diffusion directly weakens adjacent fault patches, dictating the spatiotemporal migration of seismicity. We conclude that near‐real‐time monitoring of seismic attenuation may help detect fluid redistribution in active fault systems and may provide useful information for time‐dependent seismic hazard assessment.

Suggested Citation

Malagnini, L., Lucente, F.P., Munafo, I., Dreger, D.S., Parsons, T.E., and Burgmann, R., 2026, Temporal and spatial changes in seismic attenuation associated with inferred fluid migration in the 2016 central Apennines earthquake sequence: Bulletin of the Seismological Society of America, https://doi.org/10.1785/0120250262.

ISSN: 1943-3573 (online)

Study Area

Publication type Article
Publication Subtype Journal Article
Title Temporal and spatial changes in seismic attenuation associated with inferred fluid migration in the 2016 central Apennines earthquake sequence
Series title Bulletin of the Seismological Society of America
DOI 10.1785/0120250262
Edition Online First
Publication Date May 11, 2026
Year Published 2026
Language English
Publisher Seismological Society of America
Contributing office(s) Pacific Coastal and Marine Science Center
Country Italy
Other Geospatial central Apennines
Additional publication details