Aseismic transient during the 2010–2014 seismic swarm: evidence for longer recurrence of M ≥ 6.5 earthquakes in the Pollino gap (Southern Italy)?

Abstract In actively deforming regions, crustal deformation is accommodated by earthquakes and through a variety of transient aseismic phenomena. Here, we study the 2010–2014 Pollino (Southern Italy) swarm sequence (main shock M W 5.1) located within the Pollino seismic gap, by analysing the surface...

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Autores principales: Daniele Cheloni, Nicola D’Agostino, Giulio Selvaggi, Antonio Avallone, Gianfranco Fornaro, Roberta Giuliani, Diego Reale, Eugenio Sansosti, Pietro Tizzani
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/c2beb7b2b6b34a1d8f2d32372a26ce3e
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