A reflection seismic experiment produces the CMP gather plotted in Figure 7.21. Using the t 2(x2) method, determine the approximate rms velocity of the material overlying each reflector. Then compute...

A reflection seismic experiment produces the CMP gather plotted in Figure 7.21.

Using the t

2(x2) method, determine the approximate rms velocity of the material

overlying each reflector. Then compute an approximate depth to each reflector.

Note: You should get approximately the same velocity for each reflector; do not

attempt to solve for different velocities in the different layers.