Bulletin of the Seismological Society of America
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Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1; p. 328-333; DOI: 10.1785/0120050074
© Seismological Society of America
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Figure 001


Figure 1. A schematic diagram showing ray paths of major seismic phases commonly used in crustal receiver functions. P-wave receiver functions emphasize the PpPmp phase on the vertical component, whereas conventional receiver functions accentuate P-to-S conversions such Ps and PsPms on horizontal components.





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