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

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 deform...

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Xehetasun bibliografikoak
Argitaratua izan da:Sci Rep
Egile Nagusiak: Cheloni, Daniele, D’Agostino, Nicola, Selvaggi, Giulio, Avallone, Antonio, Fornaro, Gianfranco, Giuliani, Roberta, Reale, Diego, Sansosti, Eugenio, Tizzani, Pietro
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Nature Publishing Group UK 2017
Gaiak:
Article
Sarrera elektronikoa:https://ncbi.nlm.nih.gov/pmc/articles/PMC5429810/
https://ncbi.nlm.nih.gov/pubmed/28404990
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-00649-z
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