Ð An estimation of local site eects in the Volvi basin as derived from observation and modeling is presented in this paper. The Volvi basin is located in the Mygdonian graben in northern Greece near the city of Thessaloniki. This test site has been studied and instrumented in the framework of thè`E URO-SEISTEST'' and``EURO-SEISMOD'' projects funded by the European Union, aimed at improving knowledge of the in¯uence of the local geology on the seismic response of a target area. In this context we calculate synthetic seismograms along a 2-D pro®le intersecting the graben, instrumented and accurately investigated with a geophysical survey and geotechnical tests. The seismic wave®eld from the source to the target area has been computed with the modal summation method, while inside two of the investigated models representing the 2-D section, the wave®eld has been numerically propagated with the ®nite-dierence method. We compare the results of the two simulations, both in the time and frequency domain. We also compare the results with experimental data related to an event recorded by the Reftek network installed in the target area. This permits a better understanding of how the structural features of the 2-D models aect the seismic wave®eld, especially in the frequency range between 2 Hz and 4 Hz, where one can observe dierences between the simulations and the observations. This means that the general features of the models are able to reproduce observed ampli®cation eects, apart from some discrepancies due to still unresolved structural features of the site.
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