Joint Inversion of Body‐Wave Receiver Function and Rayleigh‐Wave Ellipticity

In recent years, surface‐wave dispersion has been used to image lithospheric structure jointly with receiver function or Rayleigh‐wave ellipticity. Because surface‐wave dispersion is the total propagation effect of the travel path, the joint inversion relies on dense seismic arrays or high seismicity to obtain local velocity structure. However, both receiver function and Rayleigh‐wave ellipticity are single‐station measurements with localized...