Explosion, earthquake, and ambient noise recordings in a Pliocene sediment-filled valley: Inferences on seismic response properties by reference-and non-reference-site techniques (Articolo in rivista)

Type
Label
  • Explosion, earthquake, and ambient noise recordings in a Pliocene sediment-filled valley: Inferences on seismic response properties by reference-and non-reference-site techniques (Articolo in rivista) (literal)
Anno
  • 1996-01-01T00:00:00+01:00 (literal)
Alternative label
  • Malagnini, L 1; Tricarico, P 1; Rovelli, A 1; Herrmann, RB 2; Opice, S 1; Biella, G 3; deFranco, R 3 (1996)
    Explosion, earthquake, and ambient noise recordings in a Pliocene sediment-filled valley: Inferences on seismic response properties by reference-and non-reference-site techniques
    in Bulletin of the Seismological Society of America
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Malagnini, L 1; Tricarico, P 1; Rovelli, A 1; Herrmann, RB 2; Opice, S 1; Biella, G 3; deFranco, R 3 (literal)
Pagina inizio
  • 670 (literal)
Pagina fine
  • 682 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 86 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 13 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 3 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • INGV Roma Italy Saint Louis University USA Consiglio Nazionale delle Ricerche IRRS Italy; (literal)
Titolo
  • Explosion, earthquake, and ambient noise recordings in a Pliocene sediment-filled valley: Inferences on seismic response properties by reference-and non-reference-site techniques (literal)
Abstract
  • The explosion data were collected in June 1990, as part of a crustal refraction experiment carried out in the Monti Vulsini volcanic area. A linear array of 13 digital stations was deployed orthogonally to the eastern border of the Radicofani graben: 2 stations were set up on a bedrock outcrop, whereas the remaining 11 were deployed on soft sediments, 100 m apart, along a straight line toward the center of the valley. (literal)
  • Explosion, earthquake, and ambient noise recordings were collected at the eastern edge of a Pliocene sediment-filled valley, nearby the town of San Casciano dei Bagni (Tuscany, Central Italy). The anomalous amplification of amplitudes (as high as a factor of 20 between sediment and hard-rock sites) shown by classical spectral ratios were compared with results obtained by using non-reference-site techniques, like that of Nakamura (1989) and its receiver-function-like extension. (literal)
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