Model for the paper: Cause of enigmatic upper-mantle earthquakes in central Wyoming

We use a large number of high-quality arrival-time data of local and teleseismic events to determine detailed 3-D Vp isotropic and anisotropic tomography of the crust and mantle down to 750 km depth beneath Wyoming and its adjacent areas. For details, see https://doi.org/10.1785/0220230333 This dataset contains the obtained 3-D tomographic models of isotropic P-wave velocity, azimuthal anisotropy and radial anisotropy.