be visualized by, in addition to seismic tomography, mapping the deep seismic
discontinuities, like the crust-mantle boundary (Moho), the lithosphere-asthenosphere
boundary (LAB), or the discontinuities at 410 and 660 km depth. We herein present
observations of seismic discontinuities with the P and S receiver function techniques
beneath central and western Tibet along two new profiles and discuss the results in …