C. Siebert et al., Determination of molybdenum isotope fractionation by double-spike multicollector inductively coupled plasma mass spectrometry, GEOCH GEO G, 2, 2001, pp. NIL_1-NIL_16
Molybdenum isotopic compositions are precisely determined by MC-ICP-MS meas
urements using a Mo double spike. The double spike is added prior to chemic
al purification, so that the laboratory and instrumental mass fractionation
s are separated from natural mass-dependent fractionation. Fractionation is
determined on four Mo mass ratios, providing an internal consistency check
. The external standard reproducibility is at 0.06 per mil on the Mo-98/Mo-
95 ratio (2 standard deviation)). Using a normal microconcentric nebuliser
with a cyclonic spray chamber, the minimum quantity of Mo is similar to1 mu
g for high-precision results. A hydrothermal molybdenite shows fractionatio
n of -0.3 per mil on the Mo-98/Mo-95 ratio relative to our standard (Johnso
n Matthey, 1000 mug/mL (+/-0.3%) ICP standard solution, lot 602332B). Fine-
grained sediments show fractionation of 0.1 and -0.3 per mil on the the Mo-
98/Mo-95 ratio. The observed Mo isotope fractionation is small but resolvab
le with the presented high-resolution technique.