On the Isotopic Composition of Trapped Helium and Neon in Carbonaceous Chondrites
The covariance observed in the isotopic composition of primordial He, Ne and Ar in carbonaceous chondrites can be explained on the basis of simple mass-dependent fractionation.
B. Srinivasan and O. Manuel, "On the Isotopic Composition of Trapped Helium and Neon in Carbonaceous Chondrites," Earth and Planetary Science Letters, vol. 12, pp. 282-286, Elsevier Limited, Nov 1971.
The definitive version is available at https://doi.org/10.1016/0012-821X(71)90212-3
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