Figure 3. Group velocity dispersion curve (left) and receiver functions (right) jointly inverted. The blue lines are the experimental data while the red lines indicate the chosen theoretical receiver functions, corresponding to the best percent of fit

From

Delineation of Crustal Structure at VLC Seismographic Station Using Joint Inversion of Receiver Functions and Dispersion Data

Ohaegbuchu H. E., Igboekwe M. U., Chukwu G. U.

Journal of Geosciences and Geomatics. 2015, 3(4), 109-115 doi:10.12691/jgg-3-4-3