History of carbon dating

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The simplest form of isotopic age computation involves substituting three measurements into an equation of four variables, and solving for the fourth.

This results in a range of X-values for the data points representing individual minerals.It is not easily explained, in the general case, in any other way.The data points would be expected to start out on a line if certain initial conditions were met.Each such age would match the result given by the isochron.Gain or loss of In order to make the figures easy to read (and quick to draw), the examples in this paper include few data points.

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