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- W2566455338 abstract "Volcanic unrest at Campi Flegrei caldera, Southern Italy, is characterized by episodes of ground deformation, seismicity and enhanced fumarolic activity; whether its origin is purely hydrothermal or magmatic is highly debated. We have identified ground deformation patterns in strainmeter records from a heightened unrest period in late 2006, closely resembling synthetic signals from numerical simulations of shallow magma chamber replenishment and mixing. Together with other recent findings, our results depict a situation whereby periodic arrivals of deep magma feed a shallow intrusion at 3-4 km depth. These results suggest that the analysis of strainmeter records, coupled with advanced numerical simulations of magma dynamics, could lead to new approaches in imaging subsurface dynamic processes in volcanic areas." @default.
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- W2566455338 date "2017-01-21" @default.
- W2566455338 modified "2023-10-01" @default.
- W2566455338 title "Signature of magmatic processes in strainmeter records at Campi Flegrei (Italy)" @default.
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- W2566455338 doi "https://doi.org/10.1002/2016gl071875" @default.
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