Abstract
The combined techniques of inductively coupled plasma mass spectrometry (ICP-MS) and isotope dilution yield as much as a three-fold improvement in precision for trace-level rubidium determinations in geological materials over conventional isotope dilution using thermal ionization mass spectrometry (TIMS). Rubidium determinations by TIMS, precise to 0.6% (1 s.d.), are hindered by uncorrectable fractionation effects, whereas fractionation can be monitored during ICP-MS determinations, providing results as precise as 0.17% (1 s.d.). Precise rubidium data are critical for high-precision RbSr geochronology.
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