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Primitive Matter in Meteorites
1987
Symposium - International astronomical union
A large number of elements in certain meteorites have isotopic composition different from that existing in rocks of the earth or the moon. Excess amounts of some isotopes, which are radiogenic daughters, are attributed to the in situ decay of their parent nuclide. Material containing radioactive parents is believed to have been injected into the condensing solar nebula, from astrophysical sites of their production shortly before formation of these grains. Other isotopic anomalies do not show
doi:10.1017/s0074180900154506
fatcat:5br4lrufnrewtlidrcpfu2uhii