Assessing Current Seismic Hazards in Irpinia Forty Years after the 1980 Earthquake: Merging Historical Seismicity and Satellite Data about Recent Ground Movements
Author(s)
Language
English
Obiettivo Specifico
4T. Sismicità dell'Italia
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
4/11(2021)
Electronic ISSN
2076-3263
Publisher
MDPI
Pages (printed)
168
Date Issued
April 7, 2021
Alternative Location
Subjects
Abstract
Recently, a new strain rate map of Italy and the surrounding areas has been obtained by processing data acquired by the persistent scatterers (PS) of the synthetic aperture radar interferome- try (InSAR) satellites—ERS and ENVISAT—between 1990 and 2012. This map clearly shows that there is a link between the strain rate and all the shallow earthquakes (less than 15 km deep) that occurred from 1990 to today, with their epicenters being placed only in high strain rate areas (e.g., Emilia plain, NW Tuscany, Central Apennines). However, the map also presents various regions with high strain rates but in which no damaging earthquakes have occurred since 1990. One of these regions is the Apennine sector, formed by Sannio and Irpinia. This area represents one of the most important seismic districts with a well-known and recorded seismicity from Roman times up to the present day. In our study, we merged historical records with new satellite techniques that allow for the precise determination of ground movements, and then derived physical dimensions, such as strain rate. In this way, we verified that in Irpinia, the occurrence of new strong shocks—forty years after one of the strongest known seismic events in the district that occurred on the 23 November 1980, measuring Mw 6.8—is still a realistic possibility. The reason for this is that, from 1990, only areas characterized by high strain rates have hosted significant earthquakes. This picture has been also confirmed by analyzing the historical catalog of events with seismic completeness for magnitude M ≥ 6 over the last four centuries. It is easy to see that strong seismic events with magnitude M ≥ 6 generally occurred at a relatively short time distance between one another, with a period of 200 years without strong earthquakes between the years 1732 and 1930. This aspect must be considered as very important from various points of view, particularly for civil protection plans, as well as civil engineering and urban planning development.
References
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25. Vannoli, P.; Bernardi, F.; Palombo, B.; Vannucci, G.; Console, R.; Ferrari, G. New constraints shed light on strike-slip faulting beneath the southern Apennines (Italy): The 21 August 1962 Irpinia multiple earthquakes. Tectonophysics 2016, 691, 375–384.
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28. Rovida, A.; Locati, M.; Antonucci, A.; Camassi, R. (Eds.) Italian Archive of Historical Earthquake Data (ASMI); Istituto Nazionale di Geofisica e Vulcanologia (INGV): Rome, Italy, 2017.
29. Galli, P. Roman to Middle Age Earthquakes Sourced by the 1980 Irpinia Fault: Historical, Archaeoseismological, and Paleoseis- mological Hints. Geosciences 2020, 10, 286.
30. Fracassi, U.; Valensise, G. Unveiling the Sources of the Catastrophic 1456 Multiple Earthquake: Hints to an Unexplored Tectonic Mechanism in Southern Italy. Bull. Seismol. Soc. Am. 2007, 97, 725–748.
31. Marco, S.; Stein, M.; Agnon, A.; Ron, H. Long-term earthquake clustering: A 50,000 year paleoseimic record in the Dead Sea Graben. J. Geophys. Res. 1996, 101, 6179–6191.
32. Stucchi, M.; Meletti, C.; Montaldo, V.; Akinci, A.; Faccioli, E.; Gasperini, P.; Malagnini, L.; Valensise, G. Pericolosità Sismica di Riferimento per Il Territorio Nazionale MPS04; Data Set; Istituto Nazionale di Geofisica e Vulcanologia (INGV): Rome, Italy, 2004.
33. Papanikolaou, I.D.; Roberts, G. Clustering and anticlustering in the Southern Apennines as evidenced from geological fault slip-rate seismic hazard maps and the historical record. In Proceedings of the 2nd INQUA-IGCP-567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering, Corinth, Greece, 19–24 September 2011; pp. 174–177.
34. Tondi, E.; Cello, G. Spatiotemporal evolution of the Central Apennines fault system (Italy). J. Geodyn. 2003, 36, 113–128.
35. Viti, M.; Mantovani, E.; Cenni, N.; Vannucchi, A. Interaction of seismic sources in the Apennine belt. Phys. Chem. Earth 2013, 63, 25–35.
36. Bonini, M.; Corti, G.; Delle Donne, D.; Sani, F.; Piccardi, L.; Vannucci, G.; Genco, R.; Martelli, L.; Ripepe, M. Seismic sources and stress transfer interaction among axial normal faults and external thrust fronts in the Northern Apennines (Italy): A working hypothesis based on the 1916–1920 time–space cluster of earthquakes. Tectonophysics 2016, 680, 67–89.
37. Stein, R.S.; King, G.C.P.; Lin, J. Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude 5 7.4 Landers earthquake. Science 1992, 258, 1328–1332.
38. Mantovani, E.; Viti, M.; Cenni, N.; Babbuccia, D.; Tamburelli, C.; Baglione, M.; D’Intinosante, V. Seismotectonics and present seismic hazard in the Tuscany–Romagna–Marche–Umbria Apennines (Italy). J. Geodyn. 2015, 89, 1–14.
2. Farolfi, G.; Bianchini, S.; Casagli, N. Integration of GNSS and satellite InSAR data: Derivation of fine-scale vertical surface motion maps of Po Plain, Northern Apennines and Southern Alps, Italy. IEEE Trans. Geosci. Remote. Sens. 2019, 57, 319–328.
3. Farolfi, G.; Del Soldato, M.; Bianchini, S.; Casagli, N. A procedure to use GNSS data to calibrate satellite PSI data for the study of subsidence: An example from the north-western Adriatic coast (Italy). Eur. J. Remote. Sens. 2019, 52, 54–63.
4. Farolfi, G.; Del Ventisette, C. Contemporary crustal velocity field in Alpine Mediterranean area of Italy from new geodetic data. GPS Solut. 2015, 20, 715–722.
5. D’Agostino, N.; Jackson, J.A.; Dramis, F.; Funiciello, R. Interactions between mantle upwelling, drainage evolution and active normal faulting: An example from the central Apennines (Italy). Geophys. J. Int. 2001, 147, 475–497.
6. Italiano, F.; Martelli, M.; Martinelli, G.; Nucci, M. Geochemical evidence of melt intrusions along lithospheric faults of the Southern Apennines, Italy: Geodynamic and seismogenic implications. J. Geophys. Res. 2000, 105, 13569–13578.
7. Di Luccio, F.; Chiodini, G.; Caliro, S.; Cardellini, C.; Convertito, V.; Pino, N.A.; Tolomei, C.; Ventura, G. Seismic signature of active intrusions in mountain chains. Sci. Adv. 2018, 4, e1701825.
8. Chiodini, G.; Cardellini, C.; Di Luccio, F.; Selva, J.; Frondini, F.; Caliro, S.; Rosiello, A.G.; Beddini, G.; Ventura, G. Correlation between tectonic CO2 Earth degassing and seismicity is revealed by a 10-year record in the Apennines, Italy. Sci. Adv. 2020, 6, 35.
9. Doglioni, C.; Harabaglia, P.; Martinelli, G.; Mongelli, F.; Zito, G. A geodynamic model of the Southern Apennines accretionary prism. Terra Nova 1996, 8, 540–547.
10. Rosenbaum, G.; Lister, G.S. Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides. Tectonics 2004, 23, TC1013.
11. Di Bucci, D.; Corrado, S.; Naso, G. Active faults at the boundary between Central and Southern Apennines (Isernia, Italy). Tectonophysics 2002, 359, 47–63.
12. Riguzzi, F.; Crespi, M.; Devoti, R.; Doglioni, C.; Pietrantonio, G.; Pisani, A.R. Geodetic strain rate and earthquake size: New clues for seismic hazard studies. Phys. Earth Planet. Inter. 2012, 206, 67–75.
13. Devoti, R.; Esposito, A.; Pietrantonio, G.; Pisani, A.R.; Riguzzi, F. Evidence of large scale deformation patterns from GPS data in the Italian subduction boundary. Earth Planet. Sci. Lett. 2011, 311, 230–241.
14. Palano, M. On the present-day crustal stress, strain-rate fields and mantle anisotropy pattern of Italy. Geophys. J. Int. 2015, 200, 969–985.
15. Montone, P.; Mariucci, M.T. P-wave velocity, density, and vertical stress magnitude along the crustal Po Plain (Northern Italy) from sonic log drilling data. Pure Appl. Geophys. 2015, 172, 1547–1561.
16. Mastrolembo, B.; Caporali, A. Stress and strain-rate fields: A comparative analysis for the Italian territory. Boll. Geofis. Teor. Appl. 2017, 58, 265–284.
17. Farolfi, G.; Keir, D.; Corti, G.; Casagli, N. Spatial forecasting of seismicity provided from Earth observation by space satellite technology. Sci. Rep. 2020, 10, 1–7.
18. Dermanis, A.; Livieratos, E. Applications of deformation analysis in geodesy and geodynamics. Rev. Geophys. 1983, 21, 41–50.
19. Farolfi, G.; Del Ventisette, C. Strain rates in the Alpine Mediterranean region: Insights from advanced techniques of data processing. GPS Solut. 2017, 21, 1027–1036.
20. INGV—Italian Seismic Bulletin. Available online: http://terremoti.ingv.it/en/bsi (accessed on 30 January 2021).
21. Markušic, S.; Stanko, D.; Korbar, T.; Belic, N.; Penava, D.; Kordic, B. The Zagreb (Croatia) M5.5 Earthquake on 22 March 2020. Geosciences 2020, 10, 252.
22. Galli, P.; Peronace, E. New paleoseismic data from the Irpinia Fault. A different seismogenic perspective for southern Apennines (Italy). Earth Sci. Rev. 2014, 136, 175–201.
23. Pino, N.A.; Palombo, B.; Ventura, G.; Perniola, B.; Ferrari, G. Waveform modeling of historical seismograms of the 1930 Irpinia earthquake provides insight on “blind” faulting in Southern Apennines (Italy). J. Geophys. Res. 2008, 113, B05303.
24. Serva, L.; Esposito, E.; Guerrieri, L.; Porfido, S.; Vittori, E.; Comercia, V. Environmental effects from five his-torical earthquakes in southern Apennines (Italy) and macroseismic intensity assessment: Contribution to IN-QUA EEE Scale Project. Quat. Int. 2007, 173, 30–44.
25. Vannoli, P.; Bernardi, F.; Palombo, B.; Vannucci, G.; Console, R.; Ferrari, G. New constraints shed light on strike-slip faulting beneath the southern Apennines (Italy): The 21 August 1962 Irpinia multiple earthquakes. Tectonophysics 2016, 691, 375–384.
26. Rovida, A.; Locati, M.; Camassi, R.; Lolli, B.; Gasperini, P.; Antonucci, A. Italian Parametric Earthquake Catalogue (CPTI15); Version 3.0; Istituto Nazionale di Geofisica e Vulcanologia (INGV): Rome, Italy, 2021.
27. Rovida, A.; Locati, M.; Camassi, R.; Lolli, B.; Gasperini, P. The Italian earthquake catalogue CPTI15. Bull. Earthq. Eng. 2020, 18, 2953–2984.
28. Rovida, A.; Locati, M.; Antonucci, A.; Camassi, R. (Eds.) Italian Archive of Historical Earthquake Data (ASMI); Istituto Nazionale di Geofisica e Vulcanologia (INGV): Rome, Italy, 2017.
29. Galli, P. Roman to Middle Age Earthquakes Sourced by the 1980 Irpinia Fault: Historical, Archaeoseismological, and Paleoseis- mological Hints. Geosciences 2020, 10, 286.
30. Fracassi, U.; Valensise, G. Unveiling the Sources of the Catastrophic 1456 Multiple Earthquake: Hints to an Unexplored Tectonic Mechanism in Southern Italy. Bull. Seismol. Soc. Am. 2007, 97, 725–748.
31. Marco, S.; Stein, M.; Agnon, A.; Ron, H. Long-term earthquake clustering: A 50,000 year paleoseimic record in the Dead Sea Graben. J. Geophys. Res. 1996, 101, 6179–6191.
32. Stucchi, M.; Meletti, C.; Montaldo, V.; Akinci, A.; Faccioli, E.; Gasperini, P.; Malagnini, L.; Valensise, G. Pericolosità Sismica di Riferimento per Il Territorio Nazionale MPS04; Data Set; Istituto Nazionale di Geofisica e Vulcanologia (INGV): Rome, Italy, 2004.
33. Papanikolaou, I.D.; Roberts, G. Clustering and anticlustering in the Southern Apennines as evidenced from geological fault slip-rate seismic hazard maps and the historical record. In Proceedings of the 2nd INQUA-IGCP-567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering, Corinth, Greece, 19–24 September 2011; pp. 174–177.
34. Tondi, E.; Cello, G. Spatiotemporal evolution of the Central Apennines fault system (Italy). J. Geodyn. 2003, 36, 113–128.
35. Viti, M.; Mantovani, E.; Cenni, N.; Vannucchi, A. Interaction of seismic sources in the Apennine belt. Phys. Chem. Earth 2013, 63, 25–35.
36. Bonini, M.; Corti, G.; Delle Donne, D.; Sani, F.; Piccardi, L.; Vannucci, G.; Genco, R.; Martelli, L.; Ripepe, M. Seismic sources and stress transfer interaction among axial normal faults and external thrust fronts in the Northern Apennines (Italy): A working hypothesis based on the 1916–1920 time–space cluster of earthquakes. Tectonophysics 2016, 680, 67–89.
37. Stein, R.S.; King, G.C.P.; Lin, J. Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude 5 7.4 Landers earthquake. Science 1992, 258, 1328–1332.
38. Mantovani, E.; Viti, M.; Cenni, N.; Babbuccia, D.; Tamburelli, C.; Baglione, M.; D’Intinosante, V. Seismotectonics and present seismic hazard in the Tuscany–Romagna–Marche–Umbria Apennines (Italy). J. Geodyn. 2015, 89, 1–14.
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