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Ar ar dating

Ar total fusion measures ratios, making it ideal for samples known to be very argon retentive (eg. Total fusion is performed using a laser and results are commonly plotted on probability distribution diagrams or ideograms.

In order for an age to be calculated by the Ar technique, the J parameter must be known.

J value uncertainty can be minimized by constraining the geometry of the standard relative to the unknown, both vertically and horizontally.

The NMGRL does this by irradiating samples in machined aluminum disks where standards and unknowns alternate every other position.

The quantity of potassium in a rock or mineral is variable proportional to the amount of silica present.

Therefore, mafic rocks and minerals often contain less potassium than an equal amount of silicic rock or mineral.

Due to the relatively heavy atomic weight of potassium, insignificant fractionation of the different potassium isotopes occurs.

However, because each of these parameters is difficult to determine independantly, a mineral standard, or monitor, of known age is irradiated with the samples of unknown age.

The monitor flux can then be extrapolated to the samples, thereby determining their flux.

Argon loss occurs when radiogenic K by a fast neutron reaction) can be used as a proxy for potassium.

Therefore, unlike the conventional K/Ar technique, absolute abundances need not be measured.

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Ca F is also routinely irradiated and measured to determine the Ar technique relies on ratios instead of absolute quantities, we are able to extract and measure multiple aliquots of argon from a single sample.

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