Crustal anisotropy in the source area of the 2017 Puebla-Morelos Earthquake

The anisotropic data from this repository correspond to the parameters of fast polarization and normalized delay time obtained using the Shear Wave Splitting methodology from seismic events that occurred in the Puebla-Morelos area. These are separated according to each figure in the article titled Spatiotemporal variation and structural characterization of crustal anisotropy in the source area of the 2017 Puebla-Morelos Earthquake.