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- W1553314557 abstract "Abstract Past explosive and passive effusive eruptive activities of Mt. Somma-Vesuvius, Italy, are interpreted in terms of magma geochemistry and degassing processes through comparison of pre-eruptive volatile abundances, as determined through silicate melt compositions, and new experimental volatile solubility data for phonolite melt+H 2 O +NaCl+KCl+CaSO 4 ±CaCl 2 . These 200-MPa experiments reveal that small to modest levels of S in oxidized phonolitic melt have a substantial capacity to promote degassing by reducing CI solubility in melt. This reduction in Cl solubility facilitates the exsolution of CI-and S-enriched magmatic hydrosaline liquid with or without a coexisting vapor phase. Accounting for the elevated levels of S that occur in some Somma-Vesuvius melt inclusions means that S-enriched Somma-vesuvius magmas should have exsolved a Cl-and S-Charged magmatic hydrosaline liquid±vapor, significantly earlier (i.e., at greater pressure and/or as a result of lesser bulk melt differentiation) than in the compositionally similar. S-poor Somma-Vesuvius magmas. With progressive magma evolution, after initial volatile phase exsolution, more compositionally evolved versions of the earliest primitive CI-and S-rich volatile phases subsequently drove explosive plinian and sub-plinian eruptions." @default.
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- W1553314557 date "2006-01-01" @default.
- W1553314557 modified "2023-09-23" @default.
- W1553314557 title "Chapter 11 The role of sulfur in promoting magmatic degassing and volcanic eruption at Mt. Somma-Vesuvius" @default.
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- W1553314557 doi "https://doi.org/10.1016/s1871-644x(06)80025-2" @default.
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