||Icelandic Meteorological Office
Dept. of Geophysics
Synthetic seismograms for Hella, Hveragerđi, and
Reykjavík calculated for the variable slip model
shown in Figure 14.
Vx, Vy, and Vzare velociti
es in E-W, N-S, and vertical direction, respectively.
The large amplitudes at Hveragerđi and Reykjavík are Love-waves.
The small bumps in the Vx component at Hella after 12 s are
reflections from the southern boundary.