Just got a chance to look at some cross-sections for the DTX area... Convective instability appears to be present for an extended period of time, as seen by the theta-e surface folding. There also appears to be quite strong frontogenesis in that particular area, and no directional shear... This would lead me to believe that some pretty intense banding may occur in a northeast to southwest fashion.
Also of note is how all of the experimental WRF models handle this system. They deepen the system more rapidly than previously thought, as seen by the 850mb height falls. In addition, the ARW core (which is usually drier) outputs over an inch of QPF into the cold sector just north of the thermal gradient.
Making this tricky is the very tight thermal gradient, and narrow warm intrusions seen on the cross-sections.
All in all, I would call for a general 2-4 inches north of a line from KMTC to KJXN. However, I would not at all be surprised to see significantly higher amounts depending on the verification of banding and how the thermal profile sets up. Another aspect to note is the NAM snowfall algorithm outputting +15 inches just east of MI in Ontario, Canada (before someone takes it the wrong way, I said it's something interesting to note).
While many are pushing this system off as a dud, I'm starting to think we might be looking at a "surprise snowstorm" for some areas; again, being highly dependent on certain features (wouldn't be confident enough to issue a watch... or tell a viewing audience).