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- W2601651489 abstract "Abstract Vesuvius is a high-risk volcano and the 1631 Plinian eruption is a reference event for the next episode of explosive unrest. A complete stratigraphic and petrographic description of 1631 pyroclastics is given in this study. During the 1631 eruption a phonolite was firstly erupted followed by a tephritic phonolite and finally a phonolitic tephrite, indicating a layered magma chamber. We suggest that phonolitic basanite is a good candidate to be the primitive parental-melt of the 1631 eruption. Composition of apatite from the 1631 pyroclastics is different from those of CO" @default.
- W2601651489 created "2017-04-07" @default.
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- W2601651489 date "2017-03-15" @default.
- W2601651489 modified "2023-10-01" @default.
- W2601651489 title "Magma evolution inside the 1631 Vesuvius magma chamber and eruption triggering" @default.
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- W2601651489 doi "https://doi.org/10.1515/geo-2017-0003" @default.
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