Detailed investigations have been made of two amphibole samples where
Ar-40/Ar-39 age spectra have been interpreted to show argon diffusive
loss. Both samples display complex compositional zoning that reflects
partial major and minor element chemical re-equilibration during later
thermal events that is associated with the loss of radiogenic Ar-40.
The apparent diffusive loss age spectra in these samples are an artefa
ct of this chemical re-equilibration process. One sample additionally
shows the effect of potassium gain and contamination with a potassium-
rich phase (biotite). The resulting ages in this sample are geological
ly meaningless and the apparent fit to a theoretical diffusive loss cu
rve is coincidental. This study shows that volume diffusive loss of ar
gon appears to operate at slower rates than argon loss by chemical re-
equilibration in amphiboles.