Supported by the National Natural Science Foundation of China (Grant Nos. 40274009 and 40434009);Open Fund of Geo-detection Laboratory, Ministry of Education of China, China University of Geosciences (Grant No. GDL0607)
Based on the results of pure dispersions of Rayleigh wave tomography in the Qinghai-Tibet Plateau and its adjacent areas, taking S wave velocities from previous linear inversion as the initial model, us-ing the simula...