“…After an extensive analysis of TDGCM calculations of fragment distributions using the Q 20 and Q 30 coordinates, we were led to the conclusion that these coordinates, although very useful in describing the qualitative features of fission observables (see, e.g., [6,17]), are not ideal near, at, or beyond scission. We discovered that, no matter what reasonable prescription we used to relate the Q 20 and Q 30 coordinates to a fragment mass number, some fragment masses were severely under-represented in the yield distribution.…”