Data for "Azimuthal crustal variations and their implications on the seismic impulse response in the Valley of Mexico"

We retrieved this velocity model by joint inverting receiver functions and dispersion curves. Dispersion curves were collected from a previous study, and receiver functions were generated using teleseismic data (M>=6.0) recorded in seismic stations in the Valley of Mexico between January 2003 and January 2023. See Aguilar-Velázquez et al. (2024) for more details; the velocity model numerical validation is also available in the article.