DETAILED EVALUATION OF SITE-RESPONSE ESTIMATION METHODS ACROSS AND ALONG THE SEDIMENTARY VALLEY OF VOLVI (EURO-SEISTEST)

Using records from the EURO-SEISTEST area near Thessaloniki (Greece), we studied empirically the amplification effects of a sedimentary vall ey. One of the main advantages of this site is the very detailed knowl edge of the near-subsurface structure due to exhaustive geophysical an d geotechnical measurements and data analyses (Jongmans er al., 1998). The uniqueness of the seismological data set is the very dense networ k: 31 stations were installed perpendicular and parallel to the valley axis, with minimum interstation distances of 250 m. The mean amplific ations along both axes, estimated from 13 local events, were imaged us ing the traditional spectral ratio technique, Variations of the mean a mplifications due to the choice of different data subsets were tested by the use of up to 89 local events, supplemented by four teleseismic events offering good low-frequency resolution. Results obtained using the traditional spectral ratio technique were compared with results fr om a generalized inversion technique, the H/V ratio technique, a coda wave technique, and Nakamura's technique, Advantages and disadvantages of each method are outlined, especially from a practical point of vie w.