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<title>IAGPDS - Libros</title>
<link href="https://hdl.handle.net/10481/92849" rel="alternate"/>
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<id>https://hdl.handle.net/10481/92849</id>
<updated>2026-04-20T17:03:11Z</updated>
<dc:date>2026-04-20T17:03:11Z</dc:date>
<entry>
<title>Temporal and spatial variability of S-wave and coda attenuation in the Central Apennines, Italy</title>
<link href="https://hdl.handle.net/10481/102671" rel="alternate"/>
<author>
<name>Gabrielli, Simona</name>
</author>
<author>
<name>Akinci, Aybige</name>
</author>
<author>
<name>Del Pezzo, Edoardo</name>
</author>
<id>https://hdl.handle.net/10481/102671</id>
<updated>2025-02-25T11:01:40Z</updated>
<summary type="text">Temporal and spatial variability of S-wave and coda attenuation in the Central Apennines, Italy
Gabrielli, Simona; Akinci, Aybige; Del Pezzo, Edoardo
The central Apennines are notoriously subject to important seismic sequences, such as the 2009 and 2016–2017, L’Aquila, Amatrice-Visso-Norcia (AVN) sequences, respectively. Here, we examine the temporal and spatial variation of the S-wave attenuation in Central Italy over a period from 2011 to 2017, including the AVN sequence. First, we computed the S-wave attenuation (Qβ) as a function of frequency Q(f) using the coda normalization method. Then, to visualize the spatial variation of the attenuation over time, we calculated the attenuation of coda waves using a novel 2D kernel-based function over the study area. Our results showed a 13% variation in S-wave attenuation between the pre-sequence (2011–2016) and the sequence phase, with a significant 37% decrease in Q (increase in attenuation) detected during the Visso period. Spatially, a high attenuation anomaly aligns with the Monti Sibillini thrust formation, while in time, we observed a northward migration of this high attenuation during the Norcia phase. Temporal variation in the crustal S-wave attenuation and its frequency dependence may be linked to fluid movement and fracturing developed during the AVN sequence. Coda-Q mapping confirmed an increase in attenuation during the sequence within the fault plane zones. Additionally, the broader area of interest reveals a northward extension of high attenuation, following the NS direction of the Monti Sibillini thrust.
This work has been carried out in the framework of the project SECURE Pianeta Dinamico/2023–2025 supported by Ministero dell’Istruzione, dell’Università e della Ricerca (MIUR).; The Supplementary Material for this article can be found online at: &#13;
https://www.frontiersin.org/articles/10.3389/feart.2024.1487797/full#supplementary-material
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