The thermal evolution of the Phlegraean magmatic system (southern Italy) is studied by analyzing the influence of the thermal property variations on the solution of the heat conduction equation. The aim of this paper is to verify if appropriate choices of thermal parameters can reproduce, at least to greater depths, the high temperatures measured in the geothermal wells, drilled inside the caldera, under the assumption of heat loss from a magma chamber by conduction. Since the main purpose is to verify the plausibility of such an assumption, rather simple models of the magmatic system are adopted and only major volcanic events (i.e., the Campanian Ignimbrite and the Neapolitan Yellow Tuff eruptions) are considered. The results of the simula...
The heat flow and distribution of temperatures at depth in the Campania region were analysed and cor...
A thermal modeling of the Vesuvius is presented, based on its magmatic and volcanic history. A 2D n...
Detecting volcanic unrest is of primary importance for eruption forecasting, especially on volcanoes...
The thermal evolution of the Phlegraean magmatic system (southern Italy) is studied by analyzing the...
The thermal evolution of the Phlegraean magmatic system (southern Italy) is studied by analyzing the...
A series of 2-D conductive/convective numerical models show a rather limited range of possible magma...
We illustrate a quantitative conductive/convective thermal model incorporating a wide range of geoph...
Volcanic and geothermal aspects both exist in many geologically young areas. In these areas the heat...
The last eruptive event at Mt. Vesuvius occurred in 1944 AD, ending a cycle of continuous eruptive ...
Soil-temperature measurements can provide information on the distribution of degassing fissures, the...
Few studies have detailed the thermal architecture of large-volume pyroclastic density current depos...
The Phlegrean Fields is an active caldera structure, located on the periphery of Naples (Italy. Afte...
The heat flow and distribution of temperatures at depth in the Campania region were analysed and cor...
A thermal modeling of the Vesuvius is presented, based on its magmatic and volcanic history. A 2D n...
Detecting volcanic unrest is of primary importance for eruption forecasting, especially on volcanoes...
The thermal evolution of the Phlegraean magmatic system (southern Italy) is studied by analyzing the...
The thermal evolution of the Phlegraean magmatic system (southern Italy) is studied by analyzing the...
A series of 2-D conductive/convective numerical models show a rather limited range of possible magma...
We illustrate a quantitative conductive/convective thermal model incorporating a wide range of geoph...
Volcanic and geothermal aspects both exist in many geologically young areas. In these areas the heat...
The last eruptive event at Mt. Vesuvius occurred in 1944 AD, ending a cycle of continuous eruptive ...
Soil-temperature measurements can provide information on the distribution of degassing fissures, the...
Few studies have detailed the thermal architecture of large-volume pyroclastic density current depos...
The Phlegrean Fields is an active caldera structure, located on the periphery of Naples (Italy. Afte...
The heat flow and distribution of temperatures at depth in the Campania region were analysed and cor...
A thermal modeling of the Vesuvius is presented, based on its magmatic and volcanic history. A 2D n...
Detecting volcanic unrest is of primary importance for eruption forecasting, especially on volcanoes...