Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius (Articolo in rivista)

Type
Label
  • Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius (Articolo in rivista) (literal)
Anno
  • 1996-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1126/science.274.5287.592 (literal)
Alternative label
  • Zollo, A; Gasparini, P; Virieux, J; leMeur, H; deNatale, G; Biella, G; Boschi, E; Capuano, P; deFranco, R; dellAversana, P; deMatteis, R; Guerra, I; Iannaccone, G; Mirabile, L; Vilardo, G (1996)
    Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius
    in Science (N. Y., N.Y.)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Zollo, A; Gasparini, P; Virieux, J; leMeur, H; deNatale, G; Biella, G; Boschi, E; Capuano, P; deFranco, R; dellAversana, P; deMatteis, R; Guerra, I; Iannaccone, G; Mirabile, L; Vilardo, G (literal)
Pagina inizio
  • 592 (literal)
Pagina fine
  • 594 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 274 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 3 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 5287 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • CNRS SOPHIA ANTIPOLIS; Istituto Nazionale Geofisica e Vulcanologia (INGV); Consiglio Nazionale delle Ricerche (CNR); INST NAZL GEOFIS; University of Calabria; INST UNIV NAVALE (literal)
Titolo
  • Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius (literal)
Abstract
  • A two-dimensional active seismic experiment was performed on Mount Vesuvius: Explosive charges were set off at three sites, and the seismic signal along a dense line of 82 seismometers was recorded. A high-velocity basement, formed by Mesozoic carbonates, was identified 2 to 3 kilometers beneath the volcano, A slower (P-wave velocity V-P similar or equal to 3.4 to 3.8 kilometers per second) and shallower high-velocity zone under[ies the central part of the volcano. Large-amplitude late arrivals with a dominant horizontal wave motion and low-frequency content were identified as a P to S phase converted at a depth of about 10 kilometers at the top of a low-velocity zone (V-P < 3 kilometers per second), which might represent a melting zone. (literal)
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