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. 2018 May 23;4(5):eaap8306. doi: 10.1126/sciadv.aap8306

Table 3. Apparent CRE ages at nominal shielding.

All production rates were calculated using the equations of Eugster and Michel (24) for a nominal shielding of 40 g/cm2, with P21 modified to account for Na using the Na/Mg production rate at 40 g/cm2 of shielding from Hohenberg et al. (61). All production rates are based on the whole-rock composition determined by ICP-MS (see the Supplementary Materials), with SiO2 from Agee et al. (20). The weighted average ages, including production rate uncertainties, are shown in bold.

Aliquot 3He* 21Ne 38Ar 78Kr§ 83Kr
CRE age ± 2σ (Ma) CRE age ± 2σ (Ma) CRE age ± 2σ (Ma) CRE age ± 2σ (Ma) CRE age ± 2σ (Ma)
LLNL-UI-1 — ± — 4.05 ± 0.08 4.63 ± 0.16 12.26 ± 3.62 9.12 ± 3.04
LLNL-UI-2 — ± — 4.1 ± 0.08 4.76 ± 0.28 11.22 ± 1.72 8.27 ± 1.92
LLNL-UI-3 — ± — 4.05 ± 0.06 5.16 ± 0.3 13.24 ± 2.08 9.2 ± 2.36
LLNL-UI-4 2.46 ± 0.48 5.18 ± 0.24 5.09 ± 0.8 — ± — — ± —
LLNL-UI-5 2.11 ± 0.14 4.42 ± 0.22 4.8 ± 0.26 — ± — — ± —
Weighted average|| 2.14 ± 0.13 4.11 ± 0.26 4.77 ± 0.25 12.07 ± 1.24 8.73 ± 1.34
MSWD 1.96 23.43 2.63 1.13 0.23
CRE age w/ PR unc.** 2.14 ± 0.25 4.11 ± 0.49 4.77 ± 0.54 12.07 ± 1.73 8.73 ± 1.6

*Calculated using P3 = 7.54 × 10−13 mol/g per million years.

†Calculated based on total 21Ne, using P21 = 1.06 × 10−13 mol/g per million years.

‡Calculated assuming the trapped 38Ar/36Ar ratio is 0.189, using P38 = 4.78 × 10−15 mol/g per million years.

§Calculated using P78 = 1.12 × 10−17 mol/g per million years.

¶Calculated using P83 = 7.36 × 10−17 mol/g per million years.

||See the Supplementary Materials for details on weighted average calculations.

**Systematic uncertainties on cosmogenic nuclide production rates (PR unc.) are assumed to be 10%.