Annealing rates for fission tracks in apatite vary markedly as a complex fu
nction of composition-based on an experimental study of 15 well-characteriz
ed, compositionally diverse apatites, Extensive annealing data were obtaine
d in 69 experiments (durations of 1, 10, 100, and 1000 h at temperatures fr
om 75 to 100 degrees C) on each of four apatites, three with near end-membe
r occupancy of the halogen site by F, Cl, and OH, plus the well-known apati
te from Durango, Mexico. These results were supplemented by less-comprehens
ive annealing data from 12 experiments over the same range of time and temp
erature on each of the remaining 11 apatites. Measurements of initial fissi
on-track length, a parameter of considerable importance to the derivation o
f time-temperature paths from fission-track data, reveal substantial variat
ions from one apatite to another; initial lengths are best predicted from e
tch figures. Interlaboratory comparisons of data on annealing kinetics high
light discrepancies that appear to result largely from differences in the p
recision and accuracy of experimental temperatures. None of the factors pre
viously proposed as the dominant compositional controls on annealing rates
can account completely for annealing behavior over the full range of compos
itions studied. Nevertheless, relative rates of annealing among all apatite
s are highly systematic, which allows this data set to be used in its entir
ety to constrain multikinetic annealing models that predict fission-track l
engths as a function of time and temperature.