Conventional and laser microprobe measurements of S isotope ratios were made on a suite of eight natural sulfide samples to develop a well-characterized, isotopically homogeneous set of standards for in situ laser microprobe analysis. All the samples are from massive sulfide deposits in either high-grade metamorphic terranes or igneous systems. The data indicate that at the conventional sampling scale (> 1 mm), the samples are isotopically homogeneous within the analytical uncertainty of the conventional technique (::1:0.20/00). At the laser microprobe sampling scale (70-100 /-Lm), the samples are slightly heterogeneous, reflecting either actual isotope variation, imprecision associated with the laser microprobe technique, or both. A set of calibration curves was developed to standardize accurately laser microprobe data generated on unknown samples. This represents a fundamental advance in in situ laser microprobe technology and is a rigorous analytical method for accurately determining 034SCDT values from extremely small sample domains within sulfide minerals.
No takes yet. Share an insight, caveat, or question.
Crowe et al. (1996) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: