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Ground Shaking Scenario at the Historical Center of Napoli (Southern Italy) for the 1456 and 1688 Earthquakes

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Abstract

Ground motion is computed at the historical center of Napoli for the 5 December 1456 and 5 June 1688 earthquakes responsible for VIII maximum felt intensity (MCS scale). Computations are performed using the hybrid technique, which is based on the mode summation and finite difference methods. These consider the source, propagation and local site effects. The approach is fully justified by the detailed knowledge of the physical parameters of the local subsoil based on the models inferred from noise cross-correlation measurements between two receivers. Moreover, the propagation model is validated through the fitting of synthetics with recording of a moderate earthquake at the historical center of Napoli (29 December 2013, MW = 5.2) close to the seismogenic fault responsible for the 1688 earthquake. Ground motion is computed along a two-dimensional section crossing the historical center for the seismogenic sources as known from the literature. A consistency exists between the computed peak ground acceleration and intensity data if we attribute higher moment magnitudes of 7 to the 1688 earthquake and 7.3–7.4 for the 1456 earthquake. In light of the uncertainties related to the macroseismic intensities and estimated magnitudes of these historical events and the relevant masonry heritage of the historical center of Napoli, the highest values of the computed ground motion are suggested for seismic retrofitting of the masonry heritage. A scenario earthquake like those of 1688 (MW = 7) and 5 December 1456 (MW = 7.4) is predicted by the seismic code for limit states of life safety or collapse, depending on the site and the true material damping.

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References

  • Cancani, A. (1904). Sur l’emploi d’une double echelle seismique des intesites, empirique et absolue. Gerlands Beitrage Geophysik,2, 281–283.

    Google Scholar 

  • Costanzo, M. R., & Nunziata, C. (2019). VS models in the historical centre of Napoli (Southern Italy) from noise cross-correlation. Journal of Volcanology Geothermal Research,369, 80–94. https://doi.org/10.1016/j.jvolgeores.2018.11.014.

    Article  Google Scholar 

  • CPTI15. (2015). the 2015 version of the Parametric Catalogue of Italian Earthquakes. In A. Rovida, M. Locati, R. Camassi, B. Lolli and P. Gasperini (Eds.) http://emidius.mi.ingv.it/CPTI115-DBMI15. Accessed 27 Jan 2020.

  • Deino, A. L., Orsi, G., Piochi, M., & de Vita, S. (2004). The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera-Italy) assessed by 40Ar/39Ar dating method. Journal of Volcanology and Geothermal Research,133(1–4), 157–170. https://doi.org/10.1016/S0377-0273(03)00396-2.

    Article  Google Scholar 

  • Di Bucci, D., Massa, B., Tornaghi, M., & Zuppetta, A. (2006a). Structural setting of the Southern Apennine fold-and-thrust belt (Italy) at hypocentral depth: The Calore Valley case history. Journal of Geodynamics,42, 175–193.

    Article  Google Scholar 

  • Di Bucci, D., Massa, B., & Zuppetta, A. (2006b). Relay ramps in active normal fault zones: A clue to the identification of seismogenic sources (1688 Sannio earthquake, Italy). Geological Society of America Bulletin,118(3–4), 430–448. https://doi.org/10.1130/B25783.1.

    Article  Google Scholar 

  • Di Donato, V., Ruello, M. R., Liuzza, V., Carsana, V., Giampaola, D., Di Vito, M., et al. (2018). Development and decline of the ancient harbor of Napoli. Geoarcheology. https://doi.org/10.1002/gea.21673.

    Article  Google Scholar 

  • DISS. (2018). Database of Individual Seismogenic Sources (DISS), Version 3.2.1: A compilation of potential sources for earthquakes larger than M 5.5 in Italy and surrounding areas. Istituto Nazionale di Geofisica e Vulcanologia. https://doi.org/10.6092/ingv.it-diss3.2.1. http://diss.rm.ingv.it/diss/. Accessed 27 Jan 2020.

  • Fäh, D., & Panza, G. F. (1994). Realistic modelling of observed seismic motion in complex sedimentary basins. Annali di Geofisica,3, 1771–1797.

    Google Scholar 

  • Fracassi, U., & Valensise, G. (2007). Unveiling the sources of the catastrophic 1456 multiple earthquake: Hints to an unexplored tectonic mechanism in Southern Italy. Bulletin of the Seismological Society of America,97(3), 725–748. https://doi.org/10.1785/0120050250.

    Article  Google Scholar 

  • Gasperini, P., Bernardini, F., Valensise, G., & Boschi, E. (1999). Defining seismogenic sources from historical earthquake felt reports. Bulletin of the Seismological Society of America,89, 94–110.

    Google Scholar 

  • Guidoboni, E., Ferrari, G., Mariotti, D., Comastri, A., Tarabusi, G., Sgattoni, G., & Valensise, G. (2018). CFTI5Med, Catalogo dei Forti Terremoti in Italia (461 a.C.-1997) e nell’area Mediterranea (760 a.C.-1500). Istituto Nazionale di Geofisica e Vulcanologia (INGV). https://doi.org/10.6092/ingv.it-cfti5. http://storing.ingv.it/cfti/cfti5/. Accessed 27 Jan 2020.

  • Gusev, A. A. (1983). Descriptive statistical model of earthquake source radiation and its application to an estimation of short period strong motion. Geophysics Journal of the Royal Astronomical Society,74, 787–800.

    Google Scholar 

  • Liuzza, V. (2014). Ricostruzione paleogeografica e paleoambientale della città di Napoli: Un’indagine geoarcheologica. Tesi di Dottorato in Scienze della Terra, XXVI ciclo. Università degli Studi di Napoli Federico II, p. 390. Retrieved from http://www.fedoa.unina.it/id/eprint/9801. Accessed 27 Jan 2020.

  • NTC2018, Aggiornamento delle Norme Tecniche per le Costruzioni, D.M.17.01.2018, G.U. n.42 del 20.02.2018, Suppl. Ord. n.8.

  • Nunziata, C. (2004). Seismic ground motion in Napoli for the 1980 Irpinia earthquake. Pageoph,161(5/6), 1239–1264.

    Article  Google Scholar 

  • Nunziata, C., Costa, G., Marrara, F., & Panza, G. F. (2000). Validated estimation of the response spectra for the 1980 Irpinia earthquake in the eastern area of Napoli. Earthquake Spectra,16(3), 643–660.

    Article  Google Scholar 

  • Nunziata, C., Natale, M., & Panza, G. F. (2004). Seismic characterization of neapolitan soils. Pageoph,161(5/6), 1285–1300.

    Article  Google Scholar 

  • Nunziata, C., Sacco, C., & Panza, G. F. (2011). Modeling of ground motion at Napoli for the 1688 scenario earthquake. Pure and Applied Geophysics,168, 495–508.

    Article  Google Scholar 

  • Panza, G. F., La Mura, C., Peresan, A., Romanelli, F., & Vaccari, F. (2012). Seismic hazard scenarios as preventive tools for a disaster resilient society. In R. Dmowska (Ed.), Advances in geophysics (pp. 93–165). London: Elsevier.

    Google Scholar 

  • Panza, G. F., Paskaleva, I., & Nunziata, C. (Eds.). (2004). Pure and applied geophysics, topical volume “seismic ground motion in large urban areas” (pp. 943–948). Basel: Birkhauser.

    Google Scholar 

  • Perrotta, A., Scarpati, C., Luongo, G., & Morra, V. (2006). The Campi Flegrei caldera boundary in the city of Naples. In B. De Vivo (Ed.), Volcanism in the campania plain: Vesuvius (pp. 85–96). Campi Flegrei and Ignimbrites: Elsevier.

    Chapter  Google Scholar 

  • Pondrelli, S. (2002). European-mediterranean regional centroid-moment tensors catalog (RCMT).  Istituto Nazionale di Geofisica e Vulcanologia. https://doi.org/10.13127/rcmt/euromed.

  • Scarpati, C., Perrotta, A., Lepore, S., & Calvert, A. (2013). Eruptive history of Neapolitan volcanoes: Constraints from 40Ar–39Ar dating. Geological Magazine,150(3), 412–425. https://doi.org/10.1017/S0016756812000854.

    Article  Google Scholar 

  • Valensise, G., & Pantosti, D. (2001). Database of potential sources for earthquakes larger than M 5.5 in Italy. Annali di Geofisica, Istituto Nazionale di Geofisica e Vulcanologia,44(4), 1–180.

    Google Scholar 

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Acknowledgements

We thank two anonymous reviewers for the useful comments. Many thanks to Prof. G.F. Panza and Prof. F. Romanelli and the Seismology Group of the Trieste University for the use of programs for Love and Rayleigh modal summation computation.

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Correspondence to C. Nunziata.

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Nunziata, C., Costanzo, M.R. Ground Shaking Scenario at the Historical Center of Napoli (Southern Italy) for the 1456 and 1688 Earthquakes. Pure Appl. Geophys. 177, 3175–3190 (2020). https://doi.org/10.1007/s00024-020-02426-y

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