GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.3 GNGTS 2024 The combined long-term horizontal velocity feld is then used for obtaining the strain-rate feld across the actve deformaton zones, by applying the classic approach based on GNSS velocity vectors converted in the strain-rate feld (e.g., Beavan and Haines, 2001; Shen-Tu, 1998). References Altamimi Z., Métvier L., Rebischung P., Rouby H., Collilieux X.; 2017: ITRF2014 plate moton model, Geophys. J. Int., 209, 3, doi:10.1093/gji/ggx136. Beavan J., Haines J.; 2001: Contemporary horizontal velocity and strain rate felds on the Pacifc- Australian plate boundary zone through New Zealand. J. Geophys. Res., 106(B1), doi:10.1029/2000JB900302. Devot R., D’Agostno N., Serpelloni E., Pietrantonio G., Riguzzi F., Avallone A., Cavaliere A., Cheloni D., Cecere G., D’Ambrosio C., Falco L., Selvaggi G., Mètois M., Esposito A., Sepe V., Galvani A., Anzidei M.; 2017: A Combined Velocity Field of the Mediterranean Region. Annals of Geophysics, 60(2), doi:10.4401/ag-7059. Shen-Tu B., Holt W.E., Haines J.; 1998: Contemporary kinematcs of the western United States determined from earthquake moment tensors, very long baseline interferometry, and GPS observatons. J. Geophys. Res., 103(B8), doi:10.1029/98JB01669. Corresponding author: alessandro.galvani@ingv.it