Site characterization in Durrës (Albania) from a seismic microzonation perspective

Twenty-nine single-station noise measurements, processed through the HVSR technique, a MASW survey and two 2D array measurements were performed in Durrës to provide useful elements for a geophysical subsoil characterization. Results from noise measurements defined a zone eastward of the historical centre, where the characteristics of shallow soil layers are responsible for modification to the seismic demand. In particular, HVSR curves in this area showed amplitude higher than 3.4 at a period higher than 1s. From the analysis of the collected data, four different groups of HVSR curves were recognized, whereas noise measurements were also used to retrieve a preliminary bedrock depth map. These results are potentially useful for correlating construction typologies and period vibration of the buildings with the site amplification and with the damages observed during the seismic sequence for which the highest magnitude event was the MW 6.2 November 26th, 2019. Moreover, two shear waves velocity Vs profiles were obtained from a joint inversion of Rayleigh curves with ellipticity. In one case, it revealed the presence of a soil of very poor mechanical properties, which was classified as D soil according to the international codes (EC8, NEHRP); in the other case, the Vs profile allowed to retrieve important information about the seismic bedrock to be used in numerical modeling for the third level of seismic microzonation