Jan 16-18? That was a beefy clipper, no? An anafront is an actual cold front, with precipitation embedded behind the front. This happens when the front tilts back westard with height, giving an isentropic slope for air to rise along. I think, in the Carolinas at least, our woes with these are largely because the mountains make this structure near impossible to maintain. Surface cold front air in this sort of orientation will be stable (the backwards tilt implies a low level inversion near the surface front), which means it ain't making it over the mountains and the cold air aloft catches up.