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At Degelen Mountain in Kazakhstan, seismic data were collected between the ground surface and tunnel 160, and the travel times of the P-waves were processed with tomographic methods to estimate the velocities. Most of the estimated velocities were between 4000 and 5150m/s. The tomogram showed two distinct regions with low velocities: One region was near the tunnel between 216 and 270 m, horizontal distance (measured from the tunnel portal). The other region was near the ground surface between 310 and 424 m, horizontal distance; this particular region had the lowest velocities in the tomogram. An analysis of the resolution indicated that the smallest features that could be detected were about 18m across. Near the middle of the tomogram, features were well resolved in the horizontal direction but just moderately resolved in the vertical direction. Near the edges of the tomogram, features were poorly resolved.

Processing of seismic tomography data collected at Tunnel 160, Deglen Mountain, Kazakhstan