Slab-Plume Interaction and 2013 Wyoming Upper-Mantle Earthquakes

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