Slab-Plume Interaction and 2013 Wyoming Upper-Mantle Earthquakes

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. This dataset contains: (1) Arrival time data of local/regional earthquakes and relative travel-time residuals of teleseismic events we used, (2) the obtained 3-D tomographic models of isotropic P-wave velocity, azimuthal anisotropy and radial anisotropy.