Figure 4.
Assemblage of trace‐normalized P‐wave record sections for all shotpoints on line 95‐B, plotted with a reduction velocity of 6·0 km s−1. The data have been band‐pass filtered from 2 to 12 Hz. Superimposed are the traveltimes (dashed lines) computed with ray‐tracing from the P‐wave model for line 95‐B shown in Fig. 7. The record sections are plotted together with an elevation profile along the seismic line, which also shows the locations of shotpoints and the main geological features (FL = Franconian Line, GJZ = Gera‐Jachymov Zone, exposed granulites, EL = Elbe Line).