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《Progress in Geophysics》 2008-06
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A review of the receiver function method

XU Qiang1,2,ZHAO Jun-meng1(1.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China)  
The P receiver function method and S receiver function method obtained from the teleseismic body waves have become powerful techniques in detecting the discontinuities in the crust and upper mantle underneath a seismic station.The P receiver function method is widely used in determining the S wave velocity structure of the crust,the thickness and bulk composition of the crust,the variation in the thickness of the mantle transition zone and the discontinuities in the mantle lithosphere.While the S receiver function technique,as an excellent complement for the P receiver function method,can identify the discontinuities of the mantle lithosphere(for example,Moho and LAB) using the higher resolution body waves than surface wave observations,because in the depth interval between Moho and the mantle transition zone,Sp converted phases arrive much earlier than the multiples from the shallow discontinuities,but the Ps converted are often invisible owing to the heavily disturb of multiples.In this paper,we present the application of P receiver function and S receiver function in mapping the discontinuities in the crust and upper mantle and the related research thoughts.
【Fund】： 中国科学院“百人计划”择优支持项目资助
【CateGory Index】： P315
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