Magma transfer at Campi Flegrei caldera (Italy) before the 1538 AD eruption

Calderas are collapse structures related to the emptying of magmatic reservoirs, often associated with large eruptions from long-lived magmatic systems. Understanding how magma is transferred from a magma reservoir to the surface before eruptions is a major challenge. Here we exploit the historical,...

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Detalles Bibliográficos
Autores principales: Di Vito, Mauro A., Acocella, Valerio, Aiello, Giuseppe, Barra, Diana, Battaglia, Maurizio, Carandente, Antonio, Del Gaudio, Carlo, de Vita, Sandro, Ricciardi, Giovanni P., Ricco, Ciro, Scandone, Roberto, Terrasi, Filippo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4997606/
https://www.ncbi.nlm.nih.gov/pubmed/27558276
http://dx.doi.org/10.1038/srep32245

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4997606/
https://www.ncbi.nlm.nih.gov/pubmed/27558276
http://dx.doi.org/10.1038/srep32245

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