Surface faulting on archaeological relics: a review of case histories from Dead sea to Alps. (Articolo in rivista)

Type
Label
  • Surface faulting on archaeological relics: a review of case histories from Dead sea to Alps. (Articolo in rivista) (literal)
Anno
  • 2001-01-01T00:00:00+01:00 (literal)
Alternative label
  • Galli P., Galadini F. (2001)
    Surface faulting on archaeological relics: a review of case histories from Dead sea to Alps.
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Galli P., Galadini F. (literal)
Pagina inizio
  • 291 (literal)
Pagina fine
  • 312 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
  • Tectonophysics Impact Factor 1.409 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 335 (literal)
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  • Trattasi dell'analisi delle dislocazioni di resti archeologici dovute a faglie attive, per l'attivazione durante terremoti ad elevata magnitudo. (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • 1 - Dipartimento della Protezione Civile 2 - CNR (literal)
Titolo
  • Surface faulting on archaeological relics: a review of case histories from Dead sea to Alps. (literal)
Abstract
  • We report several cases of surface faulting on archaeological relics along the Dead Sea Valley, in Crete, and in central and northern Italy. With the exception of the Fucino normal faults (central Italy), all the faulting is related to strike-slip or oblique motions. We describe only those sites for which paleoseismological or specific geological analyses had confirmed the existence of an active fault, thus omitting any ambiguous interpretation of effects attributable to other natural or anthropic phenomena. All the cases reviewed allowed us to assume the age of the faulting event and the amount of slip, thus characterising unknown or poorly known destructive earthquakes. The use of archeoseismological analyses, and particularly of the faulting of archaeological relics, always improves our knowledge of the seismicity and seismotectonics of regions for which the information about the historical seismicity and7or the geological evidence are scarce or uncertain. (literal)
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