GNGTS 2021 - Atti del 39° Convegno Nazionale

41 GNGTS 2021 S essione 1.1 The area of interest was divided into 0.5° x 0.5° square cells. Fig. 1 shows the preliminary re- sults regarding the seismic and geodetic moment-rates and the corresponding SCCs values. The SCC estimation allowed to differentiate crustal deformation modality (seismic versus aseismic), as well as to highlight possible seismic gaps over the whole region. References D’Agostino, N. (2014). Complete seismic release of tectonic strain and earthquake recurrence in the Apen- nines (Italy). Geophysical Research Letters , 41 (4), 1155-1162, doi: 10.1002/2014GL059230. Déprez, A., Doubre, C., Masson, F., & Ulrich, P. (2013). Seismic and aseismic deformation along the East African Rift System from a reanalysis of the GPS velocity field of Africa. Geophys. J. Int. , 193, 1353-1369, doi:10.1093/gji/ggt085. Hyndman, R. D., &Weichert, D. H. (1983). Seismicity and rates of relative motion on the plate boundaries of western North America. Geophysical Journal International , 72 (1), 59-82, doi: 10.1002/2014GL059230. Kostrov, V. (1974). Seismic moment and energy of earthquakes, and seismic Row of rock. Izv. Acad. Sci. USSR Phys. Solid Earth , 1, 23-44. Masson, F., Chéry, J., Hatzfeld, D., Martinod, J., Vernant, P., Tavakoli, F., & Ghafory‐Ashtiani, M. (2005). Seis- mic versus aseismic deformation in Iran inferred from earthquakes and geodetic data. Geophys. J. Int. , 160, 217-226, doi:10.1111/j.1365‐246X.2004.02465.x. Mazzotti, S., Leonard, L. J., Cassidy, J. F., Rogers, G. C., & Halchuk, S. (2011). Seismic hazard in west- ern Canada from GPS strain rates versus earthquake catalog. J. Geophys. Res. , 116, B12310, doi:10.1029/2011JB008213. Mazzotti, S., & Adams, J. (2005). Rates and uncertainties on seismic moment and deformation in eastern Canada. Journal of Geophysical Research: Solid Earth , 110 (B9), doi: 10.1029/2004JB003510. Miller, C. K., & Furlong, K. P. (1988). Thermal-mechanical controls on seismicity depth distributions in the San Andreas fault zone. Geophysical Research Letters , 15, 1429-1432. Pancha, A., Anderson, J. G., & Kreemer, C. (2006). Comparison of seismic and geodetic scalar moment rates across the Basin and Range Province. Bull. Seismol. Soc. Am. , 96, 11–32, doi:10.1785/0120040166. Palano, M., Imprescia, P., Agnon, A., & Gresta, S. (2018). An improved evaluation of the seismic/geodetic deformation‐rate ratio for the Zagros Fold‐and‐Thrust collisional belt. Geophys. J. Int. , 213, 194-209, doi:10.1093/gji/ggx524. Palano, M., Ursino, A., Spampinato, S., Sparacino, F., Polonia, A., & Gasperini, L. (2020). Crustal deforma- tion, active tectonics and seismic potential in the Sicily Channel (Central Mediterranean), along the Nubia-Eurasia plate boundary. Scientific Reports , 10, 21238, doi:10.1038/s41598-020-78063-1. Savage, J. C., & Simpson, R. W. (1997). Surface strain accumulation and the seismic moment tensor. Bulletin of the Seismological Society of America , 87 (5), 1345-1353. Sparacino, F., Palano, M., Peláez, J. A., & Fernández, J. (2020). Geodetic deformation versus seismic crustal moment-rates: insights from the Ibero-Maghrebian region. Remote Sensing , 12 (6), 952. Williams, C. F. (1996). Temperature and the seismic/aseismic transition: Observations from the 1992 Land- ers earthquake. Geophysical research letters , 23 (16), 2029-2032. Corresponding author: bruno.galuzzi@unimib.it