The development and status of the Receiver Function application
接收函数方法应用的现状及其发展

Using teleseismic PS converted waveform to get Receiver Function is one of efficient methods which can study velocity discontinuity of the crust and mantle structure under seismic station.In recent years, using SP converted waveform to establish RF can further improve the precision of velocity discontinuity of the crust and mantle structure. In recent years, the anisotropy of crust and mantle structure can be reached by using SKS'RF. With the increase of mobile and fixed seismic array data,combining RF with seismic array technique,it can give the advantaged technique guarantee to improve the precision about discontinuity.