# Calculating radiometric dating

If these two independent dates are the same, we say they are concordant.

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By using this site, you agree to the Terms of Use and Privacy Policy. Let me write it over here in a different color. And so we could make this as over 1. Ratios of stable, low mass isotopes, like those of O, S, C, and H can be used as tracers, as well as geothermometers, since fractionation of light isotopes can take place as a result of chemical process.

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I'm just going to make up these numbers. Because of the short half-life of 14 C, it is only used to date materials younger than about 70, years.

Since the half-life of Rb87 is If none of these are present, then the only alternative is to date whole rocks. We saw that in the calculating dating video.

The radiation causes charge to remain within the grains in structurally unstable "electron traps".

So let's take the natural log of our previous answer. We have our negative sign, and we have our k.

## Safe handling of radioactive material

Instead, they are a consequence of background radiation on certain minerals. This can only be done for 14 C, since we know N 0 from the atmospheric ratio, assumed to be constant through time. Rubidium 87 has a half life of 49 billion years! Most minerals will lose Ar on heating above o C - thus metamorphism can cause a loss of Ar or a partial loss of Ar which will reset the atomic clock.

This field is known as thermochronology or thermochronometry. How old is the fossil? Modern Oceanic Pb - i.

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