| 18 Gennaio 2016 | ore 11 | Simone Tarquini – INGV PI | Sala seminari – INGV Sezione di Pisa
Abstract
Lava flows are open systems which, under favorable conditions, can attain a non-equilibrium stationary state. Although this evidence is not new, the open system nature has never been fully considered in a model which accounts for both the observed dynamics and the thermal regimes of lava flow.
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