The technique described in this paper represents the modification and
combination of two previously existing methods, alkaline fusion and ne
gative thermal ion mass spectrometry (NTIMS). We have used this techni
que to analyze repeatedly a homogeneous molybdenite powder used as a r
eference standard in our laboratory. Analyses were made over a period
of 18 months, using four different calibrations of two different spike
solutions. The age of this standard reproduces at a level of +/- 0.13
%. Each individual age analysis carries an uncertainty of about 0.4% t
hat includes the uncertainty in the decay constant for Re-187. This ne
w level of resolution has allowed us to recognize real differences in
ages for two grain-size populations of molybdenite from some Archean s
amples. (C) 1998 Elsevier Science B.V.