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Publikováno v:
Journal of Seismology. 20:151-165
We attempt to model the spatial distribution of the strong ground motion for the large M = 7.0, 1954 Sofades and M = 6.8, 1957 Velestino events (southern Thessaly basin, central Greece), using the macroseismic intensities (I M M up to 9+) observed wi