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DISS 3.2.GreDaSS: Seismogenic Source GRIS051 - Rymnio Fault | ![]() |
Source Info Summary | Commentary | Pictures | References |
Comparison between observed and modeled accelerations from the 1995 mainshock for the EW component in Kozani. a) SMA1 record of the EW component. b) to e) Synthetic accelerograms computed for four different nucleation positions from the east (accelerogram 1) to the west (accelerogram 4). The best fit is for a nucleation point at eastern location.
[from Hatzfeld et al. (1998)].
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