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  • Articles  (2)
  • 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology  (2)
  • Blackwell Publishing Ltd  (1)
  • Dipartimento della Protezione Civile - Istituto Nazionale di Geofisica e Vulcanologia  (1)
  • American Meteorological Society
  • Periodicals Archive Online (PAO)
  • Springer Nature
  • Springer Science + Business Media
  • Taylor & Francis
  • 2020-2022
  • 2005-2009  (2)
  • 1960-1964
Collection
  • Articles  (2)
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  • 2020-2022
  • 2005-2009  (2)
  • 1960-1964
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  • 1
    Publication Date: 2017-04-04
    Description: Most of the ancient town of Tindari (NE, Sicily) was settled on a plateau the most surficial layer of which was made of unconsolidated material. Ongoing excavations at the archaeological site at Tindari uncovered a large portion of the decumanus which suffered deformations preliminarily assigned to coseismic effects. An analysis of the local dynamic response through the simulation of strong seismic shaking to the bedrock and modelling of spectral ratios of the bedrock-soft soil was carried out to verify the susceptibility of superficial terrains of the promontory to coseismic deformations. To perform this simulation the finite element method (FEM) was used. Four accelerometric recordings of three earthquakes of medium-high magnitude, recorded on rocky sites, were chosen to simulate the seismic shaking, using a constitutive law for the materials composing the promontory layers both of linear-elastic type and of elastoplastic type. The analysis of the linear-elastic field allowed the definition of the frequencies for which the spectral ratios of the accelerations recorded the highest amplifications; in particular the frequency range 31.5–37.2 Hz can be combined with deformation of the paved floor of the decumanus. The analysis in the elastoplastic field highlighted the zones of promontory more susceptible to suffer plasticization process. The results show that the topmost layer of the decumanus is the most susceptible to suffer plasticization. Therefore, the performed analysis lends greater support to the hypothesis that the deformations were produced by seismic shaking.
    Description: Published
    Description: 213-222
    Description: 3.10. Sismologia storica e archeosismologia
    Description: JCR Journal
    Description: reserved
    Keywords: Fourier analysis ; Elasticity and anelasticity ; Earthquake ground motions ; Site effects ; Computational seismology ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous ; 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
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    Dipartimento della Protezione Civile - Istituto Nazionale di Geofisica e Vulcanologia
    Publication Date: 2017-04-04
    Description: Il terremoto del 1908 causò una perdita irreparabile del patrimonio storico e artistico delle due città dello Stretto. Monumenti crollati e parti di monumenti superstiti demoliti dopo il terremoto, per lasciare spazio a nuove aree previste dai piani regolatori, portarono a un azzeramento impressionante dell’eredità storica urbana di Messina e di Reggio Calabria: un’eredità già depauperata da precedenti terremoti distruttivi, ma ancora fruibile prima del 1908. I danni a chiese, monasteri e palazzi sono qui descritti sulla base di relazioni ufficiali e fonti d’archivio, che mettono in luce importanti elementi della loro preesistente e poco nota vulnerabilità.
    Description: Published
    Description: 333-392
    Description: 3.10. Sismologia storica e archeosismologia
    Description: reserved
    Keywords: Messina ; Reggio Calabria ; edifici monumentali ; effetti sismici ; terremoto del 1908 ; 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology ; 05. General::05.02. Data dissemination::05.02.02. Seismological data
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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