A MASS SPECTROMETRIC STUDY OF K39/K41 ABUNDANCE VARIATIONS BY DUAL COLLECTION AND DIGITAL MEASUREMENT TECHNIQUE
Abstract
The status of K39/K41 abundance ratios in rocks and minerals is reviewed and ,he errors and corrections required in such measurements pointed out. A double-collector mass spectrometer with digital recording has been used for K30/K41 measurements in a number of granites, charnockites and zeolites. While the granites do not reveal fractionation effect, K39 deficiency has been observed in charnockites and zeolites. Possible reasons for such a fractionation are pointed out
Keywords
K-isotopes; isotope geology.
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