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- W1992648629 abstract "The Serra della Fastuca Tephra is the product of the first explosive eruption during the most recent (∼8 Ka) silicic cycle of activity at Pantelleria. It is totally made up of fallout tephra with very limited areal distribution. Stratimetrical and grain-size data have been used to define the physical parameters of the eruption. The latter are not easily definable as various critical data for peralkaline magmas are not available in the literature. An initial velocity of 62 m s−1 has been tentatively estimated assuming the volatile phase exsolved from the magma is a mixture of HF, HCl, SO2, CO2, and water, in equal molar fraction. Terminal velocity has been found not to be affected by the distance from the vent. The pressure at fragmentation depth has been estimated at around 12 bar. These parameters suggest that the eruption column did not reach great height, even during the most energetic phases. Though this eruption cannot be easily and unequivocally classified it can be considered strombolian. Lack of hydromagmatic activity has been explained in light of the shallow fragmentation depth." @default.
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- W1992648629 date "1989-10-01" @default.
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- W1992648629 title "The Serra della Fastuca Tephra at Pantelleria: Physical parameters for an explosive eruption of peralkaline magma" @default.
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- W1992648629 doi "https://doi.org/10.1016/0377-0273(89)90020-6" @default.
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