Age of Meteorites by the A40 - K40 Method

Details Age of Meteorites by the A40 - K40 Method Age of Meteorites by the A40 - K40 Method

Jan 1955

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1955phrv...97...86w&link_type=abstract

Physical Review, vol. 97, Issue 1, pp. 86-87

Physics

17

Scientific paper

The ages of two stony meteorites were determined by measuring the A40/K40 ratio using an isotopic dilution technique. With a branching ratio λeλβ=0.085 and a decay constant λ=0.55×10-9 yr-1, the ages obtained were (4.82+/-0.20)×109 and (4.58+/-0.20)×109 years.

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