High-resolution Tomography for the Upper-mantle Structure in North China by Full-waveform Inversion of Short-period Teleseismic P Wave and Its Codas

An upper-mantle structure model of the North China calculated from teleseismic P-wave data with its coda and full-waveform inversion. The model comprises three independently parameters (Vp, Vs and density). Each data file follows the format: longitude, latitude, depth (in m) and parameter value from left to right.