Direct measurement of recoil effects on <sup>40</sup>Ar/<sup>39</sup>Ar standards
Chris M. Hall
10.6084/m9.figshare.3453239.v1
https://geolsoc.figshare.com/articles/dataset/Direct_measurement_of_recoil_effects_on_sup_40_sup_Ar_sup_39_sup_Ar_standards/3453239
<p>Advances in the <sup>40</sup>Ar/<sup>39</sup>Ar method using new techniques have led to considerable efforts to improve the accuracy of the calibration of interlaboratory
standards. However, the accuracy of the method ultimately relies on the measurement of <sup>40</sup>Ar*/<sup>39</sup>Ar<sub>K</sub> ratios on standards that have been calibrated with the K–Ar method. Usually a <sup>40</sup>Ar/<sup>39</sup>Ar total gas age is assumed to equate to a K–Ar age, but this assumes that there is zero loss of <sup>39</sup>Ar due to recoil. Traditional <sup>40</sup>Ar/<sup>39</sup>Ar total gas ages are Ar retention ages and are not strictly comparable to K–Ar ages. Efforts to estimate the importance of
this effect on standards have relied on indirect evidence for <sup>39</sup>Ar recoil. We report direct measurements of <sup>39</sup>Ar recoil for primary and secondary standards using the vacuum-encapsulation technique and show that adjustments to some standard
ages may be needed. Revised ages corrected for recoil are given for hornblendes MMhb-1 and Hb3gr, biotites GA1550 and FCT-3
and sanidines FCT-2 and TCR-2. The results show that, in most cases, recoil loss exceeds that which would be expected from
grain size and geometry. Internal defects within mineral grains are likely the dominant control on the fraction of recoiled
<sup>39</sup>Ar lost from these standards.
</p>
2016-06-21 11:14:52
Ar retention ages
TCR
standard
Hb 3gr biotites GA 1550
FCT
39 Ar recoil
39 Ar
Geology