Results 11 to 20 of about 265 (177)
Annals of Geophysics, 2004 The scaling law of the seismic spectrum experimentally calculated at Mt. Vesuvius and Campi Flegrei is used to constrain the estimate of the maximum expected peak acceleration of ground motion.
S. Petrosino +3 more
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Luigi Palmieri: first scientific bases for geophysical surveillance in Mt. Vesuvius area
Annals of Geophysics, 1999 Luigi Palmieri (Faicchio 1807 -Naples 1896), was appointed Director of the Vesuvius Observatory in 1855. He rea1ized the first model of electromagnetic seismograph and the uninterrupted use at the Observatory of this instrument represented the first step
R. Nave, M. De Lucia, S. Borgstrom
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About the shallow resistivity structure of Vesuvius volcano
Annals of Geophysics, 2008 Magnetotelluric (MT) soundings performed in the past in the volcanic area of Mt. Vesuvius by two independent research groups showed in the same places MT apparent resistivity curves with very similar shape, but statically shifted by one order of ...
A. Siniscalchi +7 more
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Giuseppe Imbò and his contribution to volcano seismology
Annals of Geophysics, 1999 Together with Fusakichi Omori and Kenzo Sassa, Giuseppe Imbò is one of the founders of volcano seismology. Imbò's novel idea in volcanic tremor analysis was the introduction of what he called "numeri indici dell'intensità eruttiva" (numerical indices of ...
R. Schick
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Self-potential, geoelectric and magnetotelluric studies in Italian active volcanic areas
Annals of Geophysics, 1997 We present the results of self-potential, geoelectric and magnetotelluric studies in Italian active volcanic areas as essential contributions both to structural modeling and to hazard evaluation. On Mt. Etna and Mt.
A. Siniscalchi +6 more
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Wavefront distortion across Mt. Vesuvius observed by a seismic array
Annals of Geophysics, 2013 Local and regional earthquakes recorded at Mt. Vesuvius in 1997 and 1998 by a temporary seismic array have been analyzed with array methods to estimate slowness and backazimuth of correlated phases. The backazimuth observed for the direct P-wave has been
Danilo Galluzzo, Mario La Rocca
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Annals of Geophysics, 2013 New velocity and attenuation images of the geological structures below Mt. Vesuvius have been obtained using the programming facilities as well as the enhanced graphical power of Mathematica8TM.
Edoardo Del Pezzo, Francesca Bianco
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Annals of Geophysics, 2013 The seismic velocity and attenuation tomography images, calculated inverting respectively P-wave travel times and amplitude spectra of local VT quakes at Mt.
Edoardo Del Pezzo +4 more
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Low frequency seismic source investigation in volcanic environment: the Mt. Vesuvius atypical case [PDF]
Advances in Geosciences, 2020 We present a detailed analysis of the low frequency seismicity occurred at Mt. Vesuvius in the time range 2003–2018. This kind of seismicity is atypical for the volcano and poorly studied, therefore we characterized it in terms of spectral analysis ...
S. Petrosino, P. Cusano
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Annals of Geophysics, 1998 In order to put new constrains on magnetic effects associated with mechanical stresses, high frequency monitoring of the geomagnetic field was carried out during a seismic tomography experiment (TOMOVES'96 project) at Mt. Vesuvius.
R. Napoli +6 more
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