Reaction of the carbonate Sibillini Mountains Basal aquifer (Central Italy) to the extensional 2016–2017 seismic sequence

Hydrogeological perturbations in response to earthquakes are widely described worldwide. In carbonate aquifers, a post-seismic discharge increase is often attributed to an increase of bulk permeability due to co-seismic fracturing and the attention on the role of faults to explain the diversion of g...

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Detalles Bibliográficos
Autores principales: Cambi, Costanza, Mirabella, Francesco, Petitta, Marco, Banzato, Francesca, Beddini, Giulio, Cardellini, Carlo, Fronzi, Davide, Mastrorillo, Lucia, Tazioli, Alberto, Valigi, Daniela
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9794788/
https://www.ncbi.nlm.nih.gov/pubmed/36575251
http://dx.doi.org/10.1038/s41598-022-26681-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9794788/
https://www.ncbi.nlm.nih.gov/pubmed/36575251
http://dx.doi.org/10.1038/s41598-022-26681-2

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