Shear wave splitting parameters used to analyze crustal anisotropy in the source region of the 2017 Puebla-Morelos Earthquake

The anisotropic data in this repository correspond to fast polarization parameters and normalized delay times obtained using the shear wave splitting methodology from seismic events that occurred in the Puebla-Morelos area. The data are organized according to each figure in the article titled "Spatiotemporal characterization of Crustal Anisotropy in the Source region of the 2017 Puebla-Morelos Earthquake."