Improving seimic hazard assessment in the Mediterranean Region
Language
English
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
5/66 (2023)
ISSN
2037-416X
Publisher
INGV
Date Issued
2023
Alternative Location
Subjects
Abstract
This paper is intended as a short presentation of the main limitations affecting seismic hazard
assessment, revisiting possible methods available in the literature to be applied for this purpose.
The convergence of the African Plate with the Eurasian Plate is the cause of the high seismic
activity characterizing the Mediterranean region, with particular intensity in its eastern part. It is
clear that the associated seismic risk requires appropriate measures for its mitigation. Seismic risk,
the amount of resources that the community is expected to pay to earthquakes in the long term, is
the product of three factors, such as seismic hazard, vulnerability and value of the exposed goods.
As earthquakes cannot be prevented, seismic risk can be mitigated by improving our knowledge
of seismic hazard, which is largely based on statistical analysis of historical earthquake catalogs.
Nevertheless, historical records are affected by problems of reliability, completeness and shortness,
as they commonly span time lengths of the same order of magnitude or even shorter than the
inter-event time of the strongest earthquakes produced by specific seismic sources. In this respect,
alternative methods can be proposed for integrating and improving our knowledge of seismogenic
processes, and estimating both time-independent and time-dependent occurrence rates of strong
earthquakes. We propose the application of physics-based earthquake simulators, requiring the
knowledge of a robust geological-geophysical seismogenic model.
assessment, revisiting possible methods available in the literature to be applied for this purpose.
The convergence of the African Plate with the Eurasian Plate is the cause of the high seismic
activity characterizing the Mediterranean region, with particular intensity in its eastern part. It is
clear that the associated seismic risk requires appropriate measures for its mitigation. Seismic risk,
the amount of resources that the community is expected to pay to earthquakes in the long term, is
the product of three factors, such as seismic hazard, vulnerability and value of the exposed goods.
As earthquakes cannot be prevented, seismic risk can be mitigated by improving our knowledge
of seismic hazard, which is largely based on statistical analysis of historical earthquake catalogs.
Nevertheless, historical records are affected by problems of reliability, completeness and shortness,
as they commonly span time lengths of the same order of magnitude or even shorter than the
inter-event time of the strongest earthquakes produced by specific seismic sources. In this respect,
alternative methods can be proposed for integrating and improving our knowledge of seismogenic
processes, and estimating both time-independent and time-dependent occurrence rates of strong
earthquakes. We propose the application of physics-based earthquake simulators, requiring the
knowledge of a robust geological-geophysical seismogenic model.
References
Bally, A. W., L. Burbi, C. Cooper and R. Ghelardoni (1988). Balanced sections and seismic reflection profiles across
the central Apennines, Mem. Soc. Geol. It. 35, 257‑310.
Burrato, P., P. Vannoli, U. Fracassi, R. Basili and G. Valensise (2012). Is blind faulting truly invisible? Tectoniccontrolled
drainage evolution in the epicentral area of the May 2012, Emilia-Romagna earthquake sequence
(northern Italy), Ann. Geophys., 55, 4, 2012; doi:10.4401/ag-6182.
Console, R., D. Pantosti and G. D’Addezio (2002). Probabilistic approach to earthquake prediction, Ann. Geophys.,
45, 435‑449.
Console, R., M. Murru, G. Falcone and F. Catalli (2007). Stress interaction effect on the occurrence probability of
characteristic earthquakes in Central Apennines, J. Geophys. Res., 113, B08313, doi:10.1029/2007JB005418.
Console, R., Murru, M., Falcone, G. and F. Catalli (2008). Stress interaction effect on the occurrence probability of
characteristic earthquakes in Central Apennines, J. Geophys. Res., 113, B08313, doi:10.1029/2007JB005418.
Console, R., M. Murru and G. Falcone (2010). Perturbation of earthquake probability for interacting faults by static
Coulomb stress changes, J. Seismol., 14, 1 67‑77.
Console, R., P. Vannoli and R. Carluccio (2018). The Seismicity of the Central Apennines (Italy) Studied by Means of
a Physics-Based Earthquake Simulator, Geoph. J. Int., 212, 916‑929, doi:10.1093/gji/ggx451.
Console, R., R. Carluccio, M. Murru, E. Papadimitriou and V. Karakostas (2022). Physics-based simulation of
spatiotemporal patterns of earthquakes in the Corinth Gulf fault system, Bull. Seism. Soc. Am., 112, 98‑117,
doi:10.1785/0120210038.
Cosentino, D., P. Cipollari, P. Marsili and D. Scrocca (2010). Geology of the central Apennines: a regional review. In:
(Eds.) Beltrando M., A. Peccerillo, M. Mattei, S. Conticelli and C. Doglioni, The Geology of Italy: tectonics and
life along plate margins, J. Virtual Expl., 36, 12, doi:10.3809/jvirtex.2010.00223.
Davies, G., J. Griffin, F. Løvholt, S. Glimsdal, C. Harbitz, H. Kie Thio, S. Lorito, R. Basili, J. Selva, E. Geist, M. A. Baptista
(2018). A global probabilistic tsunami hazard assessment from earthquake sources, Geological Society, London,
Special Publications,456, 1, 219‑244, doi:10.1144/SP456.5.
Della Vedova, B., S. Bellani, G. Pellis and P. Squarci (2001). Deep temperatures and surface heat flow distribution.
In: Anatomy of an orogeny: the Apennines and adjacent mediterranean basins. The Netherlands: Springer,
65‑76. doi:10.1007/978‑94-015-9829-3.
DISS Working Group (2021). Database of Individual Seismogenic Sources (DISS), Version 3.3.0: A compilation of
potential sources for earthquakes larger than M 5.5 in Italy and surrounding areas. https://diss.ingv.it/, Istituto
Nazionale di Geofisica e Vulcanologia (INGV), doi:10.6092/INGV.IT‑DISS3.3.0.
Guidoboni, E., A. Comastri and G. Traina (1994). Catalogue of Ancient Earthquakes in the Mediterranean Area up to
the 10th Century, ING e SGA Storia Geofisica Ambiente, Bologna, ISBN 88-85213-06-5, 504.
Guidoboni, E. and A. Comastri (2005). Catalogue of earthquakes and tsunamis in the Mediterranean area from the
11th to the 15th century, INGV e SGA Storia Geofisica Ambiente, ISBN 88-85213-10-3, 1.037.
Hasterok, D., J. A. Halpin, A. S. Collins, M. Hand, C. Kreemer, M. G. Gard and S. Glorie (2022). New Maps of Global
Geological Provinces and Tectonic Plates, Earth‑Sci. Rev., 231, doi:10.1016/j.earscirev.2022.104069.
Mc Cann, W. R., S. P. Nishenko, L. R. Sykes and J. Krause (1979). Seismic gaps and plate tectonics: seismic potential
for maior boundaries, Pure Appl. Geophys., 117, 1082‑1147.
Meletti, C., W. Marzocchi, V. D’Amico, G. Lanzano, L. Luzi, F. Martinelli, B. Pace, A. Rovida, M. Taroni F. Visini and
MPS19 Working Group (2021). The new Italian seismic hazard model (MPS19), Ann. Geophys., 64, 1, doi:10.4401/
ag‑8579.
Nishenko, S. P. and R. Buland (1987). A generic recurrence interval distribution for earthquake forecasting, Bull.
Seismol. Soc. Am., 77, 4, 1382‑1399, doi:10.1785/BSSA0770041382.
Nomikou, P., S. Carey, D. Papanikolaou, K. Croff Bell, D. Sakellariou, M. Alexandri, K. Bejelou (2012). Submarine
volcanoes of the Kolumbo volcanic zone NE of Santorini Caldera, Greece, Glob. Planet. Change, 90‑91, 135‑151,
doi:10.1016/j.gloplacha.2012.01.001.
Pantosti, D. (2000). Earthquake recurrence through time, in “Proceeding of the Hokudan International Symposium
and School on Active Faulting”, Awaji Island, Hyogo, Japan, 17th‑26th January 2000”, 363‑365.
Pirazzoli, P. A., J. Thommeret, Y. Thommeret, J. Laborel and L. F. Montaggioni (1982). Crustal block movements from
Holocene shorelines: Crete and Antikythira (Greece), Tectonophysics, 86, 27‑43.
Reid, H.F. (1910). The Mechanics of the Earthquake, The California Earthquake of April 18, 1906, Report of the State
Investigation Commission, Vol. 2, Carnegie Institution of Washington, Washington, D.C.
Rovida, A., M. Locati, R. Camassi, B. Lolli, P. Gasperini and A. Antonucci (2022). Catalogo Parametrico dei Terremoti
Italiani (CPTI15), versione 4.0. Istituto Nazionale di Geofisica e Vulcanologia (INGV). https://doi.org/10.13127/
CPTI/CPTI15.4.
Rundle, J. B., S. Stein, A. Donnellan, D. L. Turcotte, W. Klein and C.Saylor (2021). The complex dynamics of earthquake
fault systems: new approaches to forecasting and nowcasting of earthquakes, Rep. Prog. Phys. 84, 076801,
doi:10.1088/1361‑6633/abf893.
Schmid, S. M., B. Fügenschuh, A. Kounov, L. Matenco, P. Nievergelt, R. Oberhansli, J. Pleuger, S. Schefer, R. Schuster, B.
Tomljenovic, K. Ustaszewski, D. J.J. van Hinsbergen (2020). Tectonic units of the Alpine collision zone between
Eastern Alps and western Turkey, Gondwana Res., doi: 10.1016/j.gr.2019.07.005.
Schwartz, D. P. and K. J. Coppersmith (1984). Fault behavior and characteristic earthquakes: examples from the
Wasatch and San Andreas Fault Zones, J. Geophys. Res., 89, 5681‑5698.
Serpelloni, E, A. Cavaliere, L. Martelli, F. Pintori, L. Anderlini, A. Borghi, D. Randazzo, S. Bruni, R. Devoti, P. Perfetti
and S. Cacciaguerra (2022). Surface Velocities and Strain‑Rates in the Euro‑Mediterranean Region From Massive
GPS Data Processing, Front. Earth Sci. 10:907897, doi: 10.3389/feart.2022.907897.
Shimazaki, K and T. Nakata (1980). Time‑predictable recurrence model for large earthquakes, Geophys. Res. Lett.,
7, 279‑282.
Stucchi, M., C. Meletti, V. Montaldo, A. Akinci, E. Faccioli, P. Gasperini, L. Malagnini and G. Valensise (2004).
Pericolosità sismica di riferimento per il territorio nazionale MPS04 [Data set]. Istituto Nazionale di Geofisica
e Vulcanologia (INGV), doi:10.13127/sh/mps04/ag.
Valensise, G., G. Tarabusi, E. Guidoboni and G. Ferrari (2017). The forgotten vulnerability: a geology- and historybased
approach for ranking the seismic risk of earthquake-prone communities of the Italian Apennines, Int.
J. Dis. Risk Red., 25, 289‑300, doi:10.1016/j.ijdrr.2017.09.014.
Valensise, G., P. Vannoli, P. Burrato and U. Fracassi (2020). From Historical Seismology to seismogenic source models,
20 years on: Excerpts from the Italian experience, Tectonophysics, 774, 228189, doi:10.1016/j.tecto.2019.228189.
Vannoli, P., G. Martinelli and G. Valensise (2021). The seismotectonic significance of geofluids in Italy, Frontiers in
Earth Sciences, 9, doi: 10.3389/feart.2021.579390.
Wesnouski, S. (1994). The Gutenberg-Richter or Characteristic Earthquake Distribution, Which Is It, Bull. Seismol.
Soc. Am., 84, 6, doi:10.1785/BSSA0840061940.
the central Apennines, Mem. Soc. Geol. It. 35, 257‑310.
Burrato, P., P. Vannoli, U. Fracassi, R. Basili and G. Valensise (2012). Is blind faulting truly invisible? Tectoniccontrolled
drainage evolution in the epicentral area of the May 2012, Emilia-Romagna earthquake sequence
(northern Italy), Ann. Geophys., 55, 4, 2012; doi:10.4401/ag-6182.
Console, R., D. Pantosti and G. D’Addezio (2002). Probabilistic approach to earthquake prediction, Ann. Geophys.,
45, 435‑449.
Console, R., M. Murru, G. Falcone and F. Catalli (2007). Stress interaction effect on the occurrence probability of
characteristic earthquakes in Central Apennines, J. Geophys. Res., 113, B08313, doi:10.1029/2007JB005418.
Console, R., Murru, M., Falcone, G. and F. Catalli (2008). Stress interaction effect on the occurrence probability of
characteristic earthquakes in Central Apennines, J. Geophys. Res., 113, B08313, doi:10.1029/2007JB005418.
Console, R., M. Murru and G. Falcone (2010). Perturbation of earthquake probability for interacting faults by static
Coulomb stress changes, J. Seismol., 14, 1 67‑77.
Console, R., P. Vannoli and R. Carluccio (2018). The Seismicity of the Central Apennines (Italy) Studied by Means of
a Physics-Based Earthquake Simulator, Geoph. J. Int., 212, 916‑929, doi:10.1093/gji/ggx451.
Console, R., R. Carluccio, M. Murru, E. Papadimitriou and V. Karakostas (2022). Physics-based simulation of
spatiotemporal patterns of earthquakes in the Corinth Gulf fault system, Bull. Seism. Soc. Am., 112, 98‑117,
doi:10.1785/0120210038.
Cosentino, D., P. Cipollari, P. Marsili and D. Scrocca (2010). Geology of the central Apennines: a regional review. In:
(Eds.) Beltrando M., A. Peccerillo, M. Mattei, S. Conticelli and C. Doglioni, The Geology of Italy: tectonics and
life along plate margins, J. Virtual Expl., 36, 12, doi:10.3809/jvirtex.2010.00223.
Davies, G., J. Griffin, F. Løvholt, S. Glimsdal, C. Harbitz, H. Kie Thio, S. Lorito, R. Basili, J. Selva, E. Geist, M. A. Baptista
(2018). A global probabilistic tsunami hazard assessment from earthquake sources, Geological Society, London,
Special Publications,456, 1, 219‑244, doi:10.1144/SP456.5.
Della Vedova, B., S. Bellani, G. Pellis and P. Squarci (2001). Deep temperatures and surface heat flow distribution.
In: Anatomy of an orogeny: the Apennines and adjacent mediterranean basins. The Netherlands: Springer,
65‑76. doi:10.1007/978‑94-015-9829-3.
DISS Working Group (2021). Database of Individual Seismogenic Sources (DISS), Version 3.3.0: A compilation of
potential sources for earthquakes larger than M 5.5 in Italy and surrounding areas. https://diss.ingv.it/, Istituto
Nazionale di Geofisica e Vulcanologia (INGV), doi:10.6092/INGV.IT‑DISS3.3.0.
Guidoboni, E., A. Comastri and G. Traina (1994). Catalogue of Ancient Earthquakes in the Mediterranean Area up to
the 10th Century, ING e SGA Storia Geofisica Ambiente, Bologna, ISBN 88-85213-06-5, 504.
Guidoboni, E. and A. Comastri (2005). Catalogue of earthquakes and tsunamis in the Mediterranean area from the
11th to the 15th century, INGV e SGA Storia Geofisica Ambiente, ISBN 88-85213-10-3, 1.037.
Hasterok, D., J. A. Halpin, A. S. Collins, M. Hand, C. Kreemer, M. G. Gard and S. Glorie (2022). New Maps of Global
Geological Provinces and Tectonic Plates, Earth‑Sci. Rev., 231, doi:10.1016/j.earscirev.2022.104069.
Mc Cann, W. R., S. P. Nishenko, L. R. Sykes and J. Krause (1979). Seismic gaps and plate tectonics: seismic potential
for maior boundaries, Pure Appl. Geophys., 117, 1082‑1147.
Meletti, C., W. Marzocchi, V. D’Amico, G. Lanzano, L. Luzi, F. Martinelli, B. Pace, A. Rovida, M. Taroni F. Visini and
MPS19 Working Group (2021). The new Italian seismic hazard model (MPS19), Ann. Geophys., 64, 1, doi:10.4401/
ag‑8579.
Nishenko, S. P. and R. Buland (1987). A generic recurrence interval distribution for earthquake forecasting, Bull.
Seismol. Soc. Am., 77, 4, 1382‑1399, doi:10.1785/BSSA0770041382.
Nomikou, P., S. Carey, D. Papanikolaou, K. Croff Bell, D. Sakellariou, M. Alexandri, K. Bejelou (2012). Submarine
volcanoes of the Kolumbo volcanic zone NE of Santorini Caldera, Greece, Glob. Planet. Change, 90‑91, 135‑151,
doi:10.1016/j.gloplacha.2012.01.001.
Pantosti, D. (2000). Earthquake recurrence through time, in “Proceeding of the Hokudan International Symposium
and School on Active Faulting”, Awaji Island, Hyogo, Japan, 17th‑26th January 2000”, 363‑365.
Pirazzoli, P. A., J. Thommeret, Y. Thommeret, J. Laborel and L. F. Montaggioni (1982). Crustal block movements from
Holocene shorelines: Crete and Antikythira (Greece), Tectonophysics, 86, 27‑43.
Reid, H.F. (1910). The Mechanics of the Earthquake, The California Earthquake of April 18, 1906, Report of the State
Investigation Commission, Vol. 2, Carnegie Institution of Washington, Washington, D.C.
Rovida, A., M. Locati, R. Camassi, B. Lolli, P. Gasperini and A. Antonucci (2022). Catalogo Parametrico dei Terremoti
Italiani (CPTI15), versione 4.0. Istituto Nazionale di Geofisica e Vulcanologia (INGV). https://doi.org/10.13127/
CPTI/CPTI15.4.
Rundle, J. B., S. Stein, A. Donnellan, D. L. Turcotte, W. Klein and C.Saylor (2021). The complex dynamics of earthquake
fault systems: new approaches to forecasting and nowcasting of earthquakes, Rep. Prog. Phys. 84, 076801,
doi:10.1088/1361‑6633/abf893.
Schmid, S. M., B. Fügenschuh, A. Kounov, L. Matenco, P. Nievergelt, R. Oberhansli, J. Pleuger, S. Schefer, R. Schuster, B.
Tomljenovic, K. Ustaszewski, D. J.J. van Hinsbergen (2020). Tectonic units of the Alpine collision zone between
Eastern Alps and western Turkey, Gondwana Res., doi: 10.1016/j.gr.2019.07.005.
Schwartz, D. P. and K. J. Coppersmith (1984). Fault behavior and characteristic earthquakes: examples from the
Wasatch and San Andreas Fault Zones, J. Geophys. Res., 89, 5681‑5698.
Serpelloni, E, A. Cavaliere, L. Martelli, F. Pintori, L. Anderlini, A. Borghi, D. Randazzo, S. Bruni, R. Devoti, P. Perfetti
and S. Cacciaguerra (2022). Surface Velocities and Strain‑Rates in the Euro‑Mediterranean Region From Massive
GPS Data Processing, Front. Earth Sci. 10:907897, doi: 10.3389/feart.2022.907897.
Shimazaki, K and T. Nakata (1980). Time‑predictable recurrence model for large earthquakes, Geophys. Res. Lett.,
7, 279‑282.
Stucchi, M., C. Meletti, V. Montaldo, A. Akinci, E. Faccioli, P. Gasperini, L. Malagnini and G. Valensise (2004).
Pericolosità sismica di riferimento per il territorio nazionale MPS04 [Data set]. Istituto Nazionale di Geofisica
e Vulcanologia (INGV), doi:10.13127/sh/mps04/ag.
Valensise, G., G. Tarabusi, E. Guidoboni and G. Ferrari (2017). The forgotten vulnerability: a geology- and historybased
approach for ranking the seismic risk of earthquake-prone communities of the Italian Apennines, Int.
J. Dis. Risk Red., 25, 289‑300, doi:10.1016/j.ijdrr.2017.09.014.
Valensise, G., P. Vannoli, P. Burrato and U. Fracassi (2020). From Historical Seismology to seismogenic source models,
20 years on: Excerpts from the Italian experience, Tectonophysics, 774, 228189, doi:10.1016/j.tecto.2019.228189.
Vannoli, P., G. Martinelli and G. Valensise (2021). The seismotectonic significance of geofluids in Italy, Frontiers in
Earth Sciences, 9, doi: 10.3389/feart.2021.579390.
Wesnouski, S. (1994). The Gutenberg-Richter or Characteristic Earthquake Distribution, Which Is It, Bull. Seismol.
Soc. Am., 84, 6, doi:10.1785/BSSA0840061940.
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