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continue to trace headwaves along a boundary even if the
velocity contrast across the interface is no longer positive,
in which case headwaves emerge parallel to the boundary (idiff=1);
if idiff=2, initiate a headwave ray group even if there is no
critical point (or it is not found) to model diffractions along
the top of a low-velocity layer (default: 0)
Ingo Pecher
Sat Mar 7 19:13:54 EST 1998