1,721,511 research outputs found
Guidebook of the field excursion to Vesuvius, Pompei, Meta di Sorrento. Accademia Naz.le Lincei e CNR, Marzo 1979, Roma,
No full textGuida vulcanologic
A model of the Phlegraean Fields magma chamber in the last 10,500 years
No full textAbstract
Volcanological and petrological data suggest that the Phlegraean Fields volcanic activity has been fed, at least in the last 10,500 years, by a not-refilled magma chamber where trachytic residual liquids were produced by fractionation of a trachybasaltic magma. Using estimated volumes of the erupted products and P-T data obtained through petrological studies, a conductive thermal model of the chamber was built up in order to estimate its past and present size. Results suggest a volume decrease from approximately 14 to 1.4 km3 of the trachybasaltic magma in 10,500 years. Trachytic liquid would also be present in the chamber in a minimum amount of 0.4 km3. The model allowed some insights on the petrogenesis of the Phlegraean trachytes, suggesting that they were erupted as liquids because thermally buffered within the magma chamber. © 1984 Intern. Association of Volcanology and Chemistry of the Earth's Interior
The 2007 Stromboli Eruption, Special Issue Journal of Volcanology and Geothermal Research
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