A recent laboratory study of fission track
annealing by Barbarand et al. (Chemical Geology, 198, 2003, 107-137)
claimed that “etch pit size is a valuable estimator of annealing
rate of an individual apatite grain”, which could be used
instead of chlorine content to assess differential annealing between
different apatite grains. This echoes earlier suggestions that
etch pit size provides a practical alternative or even a better
approach than using Chlorine (e.g. Burtner et al., AAPG Bulletin,
78, 1994, 1613-1636). As explained in detail in the
accompanying
article (pdf), we believe that chlorine provides a much better
indicator of annealing properties, and that the data provided
by Barbarand et al. demonstrate this point clearly.