摘要
///Using tele-seismograms from stations in the region along and surrounding the Longmenshan Fault Zone, the authors stacked receiver functions by means of time-domain iterative deconvolution, further estimated Moho depths beneath the stations through the H-Kappa stacking method, and finally derived the distribution of both the Moho depth and the wave-to-velocity ratio (Vp/Vs), and their errors for the region. The result suggests that the Moho depth distribution has an outline similar to that from previous studies. A preliminary explanation is that the abnormalities of the medium to high Vp/Vs ratios on the Sichuan Basin side and on the Tibetan Plateau side are related to the water-bearing stratigraphic formations beneath the basin and to the low-velocity layers (or the channel flow) in the crust of the plateau, respectively.