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Items: 4

1.

Caldera resurgence driven by magma viscosity contrasts.

Galetto F, Acocella V, Caricchi L.

Nat Commun. 2017 Nov 24;8(1):1750. doi: 10.1038/s41467-017-01632-y.

2.

Thermally-assisted Magma Emplacement Explains Restless Calderas.

Amoruso A, Crescentini L, D'Antonio M, Acocella V.

Sci Rep. 2017 Aug 11;7(1):7948. doi: 10.1038/s41598-017-08638-y.

3.

Magmas near the critical degassing pressure drive volcanic unrest towards a critical state.

Chiodini G, Paonita A, Aiuppa A, Costa A, Caliro S, De Martino P, Acocella V, Vandemeulebrouck J.

Nat Commun. 2016 Dec 20;7:13712. doi: 10.1038/ncomms13712.

4.

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

Di Vito MA, Acocella V, Aiello G, Barra D, Battaglia M, Carandente A, Del Gaudio C, de Vita S, Ricciardi GP, Ricco C, Scandone R, Terrasi F.

Sci Rep. 2016 Aug 25;6:32245. doi: 10.1038/srep32245.

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