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This technique allows the errors involved in K-Ar dating to be checked.

Argon–argon dating has the advantage of not requiring determinations of potassium.

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The abundance of Ar is unlikely to provide the age of intrusions of granite as the age typically reflects the time when a mineral cooled through its closure temperature.

However, in a metamorphic rock that has not exceeded its closure temperature the age likely dates the crystallization of the mineral.

Thus, a granite containing all three minerals will record three different "ages" of emplacement as it cools down through these closure temperatures.

Thus, although a crystallization age is not recorded, the information is still useful in constructing the thermal history of the rock.

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