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isotone and the intercept of the line with the wero abacrber axis
represents the relative amount of that isotope present in a
mixture,

The advantaze of this method lies in its applicability to low
counting levels. This is possible because the line slope can be
determined from light absorbers rather than the heavy absorbers
required for Feather analyses. Tne method is in tentative use
for isotope characterization for mixtures of isotopes and should
be applicable to determination of Sr®?/2° ratios.

mee Cf
UNCLASSIFIED

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