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Rock samples are recorded, marked, sealed and kept free of contamination and excessive heat on the way to the lab.

The rock samples are crushed, in clean equipment, to a size that preserves whole grains of the mineral to be dated, then sieved to help concentrate these grains of the target mineral.

The method relies on satisfying some important assumptions: Given careful work in the field and in the lab, these assumptions can be met.

The rock sample to be dated must be chosen very carefully.

So assuming that no air gets into a mineral grain when it first forms, it has zero argon content.

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