Physics
Scientific paper
Feb 1957
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1957phrv..105..765s&link_type=abstract
Physical Review, vol. 105, Issue 3, pp. 765-766
Physics
1
Scientific paper
It is suggested that the He3: He4 ratio of iron meteorites be measured after the samples have been heated. It is anticipated that the ratio will be greater than in corresponding unheated samples. Results of such experiments are of importance in dating the breakup of the meteorite's parent planet as well as for estimating the value of the prehistoric cosmic-ray flux.
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