Results 71 to 80 of about 355 (168)
Noise‐based seismic monitoring of the Campi Flegrei caldera
AbstractThe Campi Flegrei caldera is one of the highest risk volcanic fields worldwide, because of its eruptive history and the large population hosted within the caldera. It experiences bradiseismic crises: sudden uplift with low energetic seismic swarm occurrences. No seismicity is recorded out of these deformation rate changes.
Lucia Zaccarelli, Francesca Bianco
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Hydrothermal instability and ground displacement at the Campi Flegrei caldera
Ground deformation is commonly observed at active volcanoes, where it represents a reliable sign of unrest and a potential precursor of eruptive activity. The source of deformation, however, is not always unequivocally constrained. Magma ascent and differentiation are generally involved, but hydrothermal fluids may play a role, due to thermal expansion
RINALDI, ANTONIO PIO +2 more
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CAMPI FLEGREI CALDERA PUMICES AND SCORIAE
[1] The Campi Flegrei (CF) caldera is one of the most dangerous quiescent volcanic systems in the world. Its activity mostly resulted in low-magnitude explosive eruptions, such as that of the Monte Nuovo tuff cone that represents the last eruptive event within the caldera (A.D. 1538).
Margherita Polacci +6 more
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Magnetotelluric investigations can reconstruct features within magmatic systems, such as the distribution of melt and fluid and the volcano-tectonic structures.
Roberto Isaia +7 more
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Understanding how volcanic systems evolve over time is a major challenge due to their complex behaviour and constantly changing conditions. This study explores a novel approach to detecting significant changes in multiparametric signals of volcanic ...
Andrea Vitale +17 more
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Caldera evolution in Campi Flegrei: the role of fractures and faults
Fractures and faults hosted in volcanic rocks in Campi Flegrei were analyzed. The fracture pattern suggests a prevalence of NE-SW and NW-SE directions and secondarily N-S and E-W trends occur. Faults often appear as conjugate structures showing normal kinematics, at places associated with ductile deformation suggesting a syn-eruption deformation ...
VITALE, STEFANO, Isaia Roberto
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b value enlightens different rheological behaviour in Campi Flegrei caldera
The Campi Flegrei caldera is one of the most dangerous volcanoes in the world and since 2005 it is in unrest. Here we evaluate the 3D tomography of the b value at the Campi Flegrei volcanic area revealing a very good correlation with the structure of the
Anna Tramelli +2 more
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Brief communication: Vent opening at Campi Flegrei – clues from dyke propagation patterns [PDF]
Forecasting future vent opening position is fundamental for managing volcanic hazards, and is usually based on the spatial density of past vents or other crust weakness indicators.
J. Selva, J. Selva, N. Mangone
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Thirty years of volcano geodesy from space at Campi Flegrei caldera (Italy). [PDF]
Polcari M +6 more
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Data analysis of the unsteadily accelerating GPS and seismic records at Campi Flegrei caldera from 2000 to 2020. [PDF]
Bevilacqua A +10 more
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