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Table 6

Age determinations for CS 29497-004, using initial production ratios from: (1) log (PR)HEW: HEW predictions (this paper) for based on Farouqi et al. (2010); (2) log (PRWP1) and (3) log (PRWP2): waiting-point assumption model predictions (from Kratz et al. 2007, their Table 2, Cols. 6 and 3 resp.).

X/Y log ϵ(X/Y)obs ErrAgeobs log (PR)HEW AgeHEW log (PRWP1) AgeWP1 log (PRWP2) AgeWP2
(1) (2) (3)
[Gyr] [Gyr] [Gyr] [Gyr]

Th/Ba −1.51 ± 0.12 5.7
Th/La −0.78 ± 0.08 3.9
Th/Ce −0.97 ± 0.06 3.0
Th/Pr −0.49 ± 0.06 3.0
Th/Nd −1.14 ± 0.07 3.0
Th/Sm −0.86 ± 0.06 3.0
Th/Eu −0.50 ± 0.06 3.0 −0.375 5.8 −0.276 10.5
Th/Gd −0.85 ± 0.07 3.2
Th/Dy −1.08 ± 0.07 3.1
Th/Ho −0.40 ± 0.17 8.1
Th/Er −0.87 ± 0.11 4.9
Th/Tm 0.02 ± 0.08 3.9
Th/Hf −0.52 ± 0.07 3.0 −0.335 8.6 −0.063 21.3

Th/REE 3.5 11.99( ± 5.46)

Th/Os −1.57 ± 0.12 5.7 −1.125 20.8 −1.009 26.2
Th/Ir −1.39 ± 0.09 4.1 −1.153 11.1 −1.022 17.2
Th/Pt −1.16 ± 0.22 10.1 −1.444 −13.3 −1.585 −19.9

Th/(Os,Ir) 4.7 27.35( ± 2.26) 14.4( ± 4.6) 20.2( ± 4.3)
Th/(Os,Ir,Pt) 5.4 24.92( ± 7.74)

Th/U −1.04 ± 0.30 6.6 + 0.195 18.4 + 0.192 18.5

U/Ba −2.55 ± 0.32 4.8
U/La −1.82 ± 0.31 4.6
U/Ce −2.01 ± 0.30 4.5
U/Pr −1.53 ± 0.30 4.5
U/Nd −2.18 ± 0.30 4.5
U/Sm −1.90 ± 0.30 4.5
U/Eu −1.54 ± 0.30 4.5 −0.570 14.4 −0.468 15.9
U/Gd −1.89 ± 0.30 4.5
U/Dy −2.12 ± 0.30 4.5
U/Ho −1.44 ± 0.34 5.1
U/Er −1.91 ± 0.31 4.6
U/Tm −1.02 ± 0.31 4.6
U/Hf −1.56 ± 0.30 4.5 −0.530 15.3 −0.356 19.4

U/REE 4.6 15.29( ± 1.74)

U/Os −2.61 ± 0.32 4.7 −1.320 19.1 −1.201 20.9
U/Ir −2.43 ± 0.31 4.6 −1.348 16.1 −1.215 18.0
U/Pt −2.20 ± 0.37 5.4 −1.639 8.3 −1.777 6.3

U/(Os,Ir) 4.6 20.14( ± 0.75) 15.1( ± 4.3) 19.4( ± 1.4)
U/(Os,Ir,Pt 4.9 17.94( ± 3.69) 17.5( ± 1.5) 15.9( ± 6.0)

Notes. Errors on ages are evaluated in two different ways: the Ye variations on PRs are propagated into AgeHEW as super- and sub-scripts, while ErrAgeobs reports the observational error propagated from the observational uncertainties on the abundance ratio. For mean ages, the dispersion around the mean is also given in the corresponding age column.

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