The three traces on the right are (top) the deconvolved P wave pulse, (bottom) the initial and (middle) final fit of the starting/final models to the stacked Q-component. The numbers inicate P-SV conversions from (1) the base of the sediments (2) the Moho and (3) multiples between the free surface and the Moho.
In the left panel, the thin line is the starting model and the thick line the final model of the inversion. A pronounced Moho at a depth of 24 km is clearly visible.