Seismic waveform modeling is one of the most powerful tools for understanding Earth's structure,since it allows waveforms to be quantitatively predicted using physical source representations and a velocity model.In the late 1960s,Don Helmberger developed the foundations of generalized ray theory(GRT)using the Cagniard-de Hoop method(Helmberger,1968).This advance ushered in a new era of computing synthetic seismograms at local to teleseismic distances in applications ranging from studying strong motions generated by earthquakes to modeling Earth's interiors from basin to core.Over the