Feedback velocity structure of the mantle beneath Thailand with seismicity of the region

Within the framework of a three-dimensional P-velocity model of the mantle of the South-East Asia, considered the mantle velocity structure beneath Thailand and its surroundings with the identification of possible premises in the deep structure of the mantle for the manifestation of earthquakes in the region. The model has been obtained by application of the method of Taylor approximation of solution of seismic tomography of P-waves arrival time introduced by Geiko.