Figure 6. Chosen solution for VLC station, result of the joint inversion of receiver functions and dispersion data. The high velocity LID, centered at a depth of about 100 km, seems to reveal the presence of a subducted slab

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