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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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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2017
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| Assuntos: | |
| Acesso em linha: | 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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