Feb 1955
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1955gecoa...7...51w&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 7, Issue 1-2, pp.51-60
Physics
10
Scientific paper
The A 40 /K 40 ratios and the Pb-U ages of various co-existing potassium feldspars and uraninites were determined. It was found that with a branching ratio and a decay constant = 0.55 × 10 -9 / yr , the A 40 /K 40 ages could be brought into agreement with the Pb-U ages for samples ranging from 260 to 1860 m.y. Ko evidence was found for the loss of argon by diffusion from potassium feldspars.
Hayden R. J.
Wasserburg Gerald J.
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