In this paper we report the results of several investigations aimed at evaluating ground motion scenarios for the September 26th, 1997 Colfiorito earthquake (Mw 6.0, 09:40 UTC). We model the observed variability of ground motions and the directivity effect through synthetic scenarios which simulate an earthquake rupture propagating at constant rupture velocity (2.7 km/s). We discuss the variability of kinematic source parameters, such as the nucleation position and the rupture velocity, and how it influences the predicted ground motions and it does not account for the total standard deviation of the empirical predictive model valid for the region. Finally, we used the results from the scenario studies for the Colfiorito earthquake to integrate the probabilistic and deterministic approaches for seismic hazard assessment.
Ground motion scenarios for the 1997 Colfiorito, Central Italy, earthquake / Emolo, Antonio; G., Cultrera; G., Franceschina; F., Pacor; V., Convertito; M., Cocco; Zollo, Aldo. - In: ANNALS OF GEOPHYSICS. - ISSN 1593-5213. - 51:2/3(2008), pp. 509-525.
Ground motion scenarios for the 1997 Colfiorito, Central Italy, earthquake
EMOLO, ANTONIO;ZOLLO, ALDO
2008
Abstract
In this paper we report the results of several investigations aimed at evaluating ground motion scenarios for the September 26th, 1997 Colfiorito earthquake (Mw 6.0, 09:40 UTC). We model the observed variability of ground motions and the directivity effect through synthetic scenarios which simulate an earthquake rupture propagating at constant rupture velocity (2.7 km/s). We discuss the variability of kinematic source parameters, such as the nucleation position and the rupture velocity, and how it influences the predicted ground motions and it does not account for the total standard deviation of the empirical predictive model valid for the region. Finally, we used the results from the scenario studies for the Colfiorito earthquake to integrate the probabilistic and deterministic approaches for seismic hazard assessment.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.