Quite a large amount of teleseismic profiling has been conducted in the past 10 years or so in the Tibetan Plateau to study the lower crust upper mantle structure, yielding informative data for the geomechanic features ranging from the in depth seismic velocity image, upper mantle anisotropy and the identification of the low velocity body and layer. Along with the improvement in seismic equipment, the method has become the major means in the studies on deep seated structures in an inexpensive manner. Marked achievement has been gained in seismic tomography, the study of receiver functions and the analysis in shear wave splitting. However, room for further studies remains.