A 40 -K 40 dating

Physics

Scientific paper

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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.

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