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The amount of Argon sublimation that occurs is a function of the purity of the sample, the composition of the mother material, and a number of other factors.

These factors introduce error limits on the upper and lower bounds of dating, so that final determination of age is reliant on the environmental factors during formation, melting, and exposure to decreased pressure and/or open-air.

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Ar (argon), the atom typically remains trapped within the lattice because it is larger than the spaces between the other atoms in a mineral crystal.

But it can escape into the surrounding region when the right conditions are met, such as change in pressure and/or temperature.

Potassium is a common element found in many materials, such as micas, clay minerals, tephra, and evaporites.

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