Intense overpressurization at basaltic open-conduit volcanoes as inferred by geochemical signals: The case of the Mt. Etna December 2018 eruption-Reference-Cited by-同舟云学术

Intense overpressurization at basaltic open-conduit volcanoes as inferred by geochemical signals: The case of the Mt. Etna December 2018 eruption

Published:2021-09-03 Issue:36 Volume:7 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Paonita Antonio¹^ORCID,Liuzzo Marco¹^ORCID,Salerno Giuseppe²^ORCID,Federico Cinzia¹^ORCID,Bonfanti Piero²^ORCID,Caracausi Antonio¹^ORCID,Giuffrida Giovanni¹^ORCID,La Spina Alessandro²^ORCID,Caltabiano Tommaso²^ORCID,Gurrieri Sergio¹^ORCID,Giudice Gaetano²^ORCID

Affiliation:

1. Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Palermo, Via Ugo La Malfa 153, 90146 Palermo Italy.

2. Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Catania, Piazza Roma 2, 95125 Catania Italy.

Abstract

Magmatic fluids entering Mt. Etna volcano system from depth exceed those outgassed into atmosphere during inter-eruptive phases.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference69 articles.

1. The role of volatiles in magma chamber dynamics

2. Frequency and magnitude of volcanic eruptions controlled by magma injection and buoyancy