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Elements; January 2005; v. 1; no. 1; p. 19-24; DOI: 10.2113/gselements.1.1.19
© 2005 Mineralogical Society of America
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Volatiles in Magmatic-Volcanic Systems

Benedetto De Vivo1, Annamaria Lima1 and James D. Webster2

1 Dipartimento di Geofisica e Vulcanologia, University of Napoli
Federico II, Via Mezzocannone 8, Napoli, Italy
2 Department of Earth & Planetary Sciences, American Museum
Natural History, 79th Central Park West, New York 10024-5192, USA

Correspondence: E-mail: bdevivo{at}unina.it

The abundance and flux of volatiles are important to the hazards associated with explosive volcanic eruptions. Volatiles in magmas can be determined from investigations of melt and fluid inclusions in combination with volatile solubility data. A comparison of the newly determined solubilities of H2O, SO2, and Cl in a molten Vesuvius phonolite with the compositions of Mt. Somma-Vesuvius melt and fluid inclusions further elucidates degassing and eruptive processes for this volcano.

KEYWORDS: melt inclusions, fluid inclusions, volatiles, solubility experiments, Vesuvius




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