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《Progress In Geophysics》 2002-04
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The Receiver Function Method and Its Progress

XU Wei-wei ZHENG Tian-yu (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101, China)  
Teleseismic P waveforms contain lots of information related to P-S phase and multiples generated at the interfaces of the crustal and upper mantle, based on the data obtained from the temporary and permanent, three-component, short-period and broad-band seismic stations, the resulting receiver function method is a commonly used technique to study the crustal and upper mantle velocity structure. This method can not only evaluate the velocity distribution below the receiver station from the waveform inversion, but also search the interfaces of the crust and the upper mantle after the superimposition of the receiver function traces. The receiver functions methods are most sensitive to the shear velocity structure near the station, gross lateral variations in structure may be obtained by examining the variation in vertical velocity distribution azimuthally around the station. The receiver function method is simple and easy to implement. Besides, it has the high resolution power with the high-density deployment of the broadband flowing seismic array. This paper overviews the evolvement of the receiver function over the recent 20 years and presents some results using this method, and in the end we argues about some tendency in the study of the method.
【Fund】: 国家基础研究发展规划项目 (G19990 4 330 1)资助
【CateGory Index】: P315.6
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