here is the main result...

Velocity of compressional seismic waves in the lithosphere is presented as deviations from 1-dimensional velocity structure (IASPEI91). Colored surfaces enclose zones where deviation from 1D are over 3%, blue being fast and red being slow. This 3D distribution of velocity was obtained by inverting ~1000 measurements of travel time and ~120 measurements of polarization of the teleseismic P waves recorded by a local short-period network.

This work is also a third chapter of my PhD thesis. Text and figures may be obtained below:

• Figure 1
• Figure 2
• Figure 3
• Figure 4 is the image above. If you'd like a full-blown postscript version (~3Mb) - write me a note.
• Figure 5.
• TEXT