Magma budgets and steady-state activity of Vulcano and Stromboli

Details Magma budgets and steady-state activity of Vulcano and Stromboli Magma budgets and steady-state activity of Vulcano and Stromboli

May 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997georl..24.1043h&link_type=abstract

Geophysical Research Letters, Volume 24, Issue 9, p. 1043-1046

Physics

30

Volcanology: Eruption Mechanisms, Volcanology: Eruption Monitoring, Volcanology: Instruments And Techniques

Scientific paper

We present three models for magma budget during steady-state volcanic activity, by which non-erupted magma is emplaced as dykes or cumulates or crystallises in place. Using gas and thermal data we apply our models at Vulcano to calculate degassing, cooling and crystallisation of magma at a rate of 40-375kgs-1 within a magma body with an upper surface at a ~2km depth. At Stromboli we calculate a steady magma supply of 300-1300kgs-1 to shallow (<1km) depths.

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