Keywords
Vesuvius Volcano
adaptive media parameterization
Section
Abstract
In order to study Vesuvius Volcano (Italy), active traveltime seismic tomography algorithm with the adaptive media parameterization were applied to the TOMOVES (1994 - 1996) experiment dataset. The velocity model shows certain key features that are in a good agreement with the previous studies and geologic and geophysical data: high-velocity anomaly inside the volcano cone, low-velocity anomalies over the volcano flanks and the upwelling of the limestone basement towards East. At the same time our model shows better resolution in the upper 2 km of the crust and reveals a low-velocity anomaly at 2-4 km depth beneath the volcano edifice. The position of this anomaly coincides with the cluster of the volcano earthquakes.References
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