Publications des scientifiques de l'IRD

Zuccarello F., Schiavi Federica, Viccaro M. (2022). The eruption run-up at Mt. Etna volcano : constraining magma decompression rates and their relationships with the final eruptive energy. Earth and Planetary Science Letters, 597, 117821 [13 p.]. ISSN 0012-821X.

Titre du document
The eruption run-up at Mt. Etna volcano : constraining magma decompression rates and their relationships with the final eruptive energy
Année de publication
2022
Type de document
Article référencé dans le Web of Science WOS:000869031400008
Auteurs
Zuccarello F., Schiavi Federica, Viccaro M.
Source
Earth and Planetary Science Letters, 2022, 597, 117821 [13 p.] ISSN 0012-821X
Although explosivity is linked with high decompression rates induced by magma ascent, the quantitative relationships between decompression rate and eruption energy have yet to be properly assessed, especially for open-conduit basaltic volcanoes, where ordinary weak activity can rapidly evolve into more intense eruptions. Here, we selected three eruptions of different explosivity from Mt. Etna's recent activity to study the relationships between the observed explosive intensities and decompression rates determined through diffusion chronometry, which is based on modeling volatile diffusion along olivine -hosted melt embayments. The approach used in this study has provided important indications on differences in the timescales of decompression-driven degassing for magmas emitted with markedly distinct eruptive dynamics, starting from similar physical and chemical conditions of the magmas involved in the three eruptions. The intense paroxysmal activity at Voragine Crater on December 3, 2015, was fostered by high decompression rate (-0.36-0.74 MPa/s), slightly higher than in the less energetic paroxysm that occurred on February 19, 2013, at New South-East Crater (NSEC) (-0.14-0.29 MPa/s). Decompression rates of magmas emitted during lava fountaining are one order of magnitude greater than values obtained for the mild flank eruption that occurred in December 2018 (-0.045-0.094 MPa/s). Our results indicate that degassing kinetics controlled the intensity of activity at Mt. Etna, thus suggesting that the explosivity does not depend exclusively on the degree of overpressurization of the shallowest reservoir due to injection of gas from the deepest levels of the plumbing system.(c) 2022 Elsevier B.V. All rights reserved.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Géophysique interne [066]
Description Géographique
ITALIE
Localisation
Fonds IRD [F B010086354]
Identifiant IRD
fdi:010086354
Contact
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    Mission Science Ouverte (MSO)
    IRD - Délégation régionale Île-de-France & Ouest
    Campus Condorcet - Hôtel à projets
    8 cours des Humanités - 93322 Aubervilliers Cedex
    Horizon Pleins textes
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