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. 2017 Jul 28;7:6822. doi: 10.1038/s41598-017-06170-7

Table 1.

(a) Model Th/U ratio calculated from radiogenic 208Pb/206Pb ratio and 207Pb/235U age.

Compositional Parameters Radiogenic Isotope Ratios Isotopic Ages
An. no ThU Pbc (pg) PbPbc P207bP206b % err P207bU235 % err P206bU238 % err corr. coef. P207bP206b - ± P207bU235 - ± P206bU238
(a) (b) (b) (c) (d) (c) (d) (c) (d) (e) (d) (e) (d) (e) (d)
Lk1 (BH 14-2012)
1 0.89 1.7 6.1 0.0482 2.8 0.0639 3.0 0.009608 0.98 0.374 110 67 62.6 1.9 61.64 0.60
2 0.69 0.6 17.2 0.04778 1.0 0.0633 1.1 0.009609 0.25 0.436 88 24 62.32 0.65 61.65 0.15
3 0.55 1.1 6.9 0.0483 2.5 0.0641 2.6 0.009637 0.41 0.304 113 59 63.1 1.6 61.83 0.25
4 1.10 0.7 6.2 0.0488 3.2 0.0648 3.3 0.009620 0.45 0.327 140 75 63.7 2.1 61.72 0.27
5 0.69 0.8 23.5 0.04735 0.6 0.0628 0.6 0.009615 0.20 0.469 67 13 61.82 0.38 61.69 0.12
Dz2 (BH 12-2004)
1 n.m 0.7 0.3 0.0531 16.7 0.075 18 0.01028 1.06 0.806 332 379 74 12 65.93 0.69
2 0.72 1.5 0.6 0.051 24.0 0.065 25 0.00924 1.30 0.828 228 554 64 15 59.30 0.76
3 0.87 0.7 2.2 0.0432 7.61 0.0549 7.9 0.009225 0.47 0.707 −159 189 54.3 4.2 59.20 0.28
4 0.56 0.5 1.6 0.0465 10.5 0.059 11 0.009264 0.65 0.767 20 252 58.6 6.3 59.45 0.38
5 0.82 1.0 0.8 0.0436 18.5 0.056 19 0.009276 0.86 0.816 −135 457 55 10 59.52 0.51
Bk1 (BH 5-2006)
1 0.73 1.4 17.3 0.04780 1.0 0.0632 1.0 0.0095913 0.085 0.235 88 23 62.21 0.59 61.617 0.055
2 0.71 1.0 19.0 0.04763 0.9 0.06289 0.9 0.0095814 0.083 0.240 80 21 61.93 0.55 61.555 0.053
3 0.76 0.8 25.3 0.04757 0.7 0.06284 0.7 0.0095859 0.072 0.217 77 16 61.88 0.41 61.581 0.048
SvN (Svea mine; Am1)
1 0.73 1.0 3.6 0.0481 4.6 0.0635 4.7 0.009595 0.35 0.237 104 109 62.6 2.8 61.56 0.21
2 0.70 0.9 11.2 0.04788 1.5 0.0633 1.5 0.009602 0.12 0.242 92 35 62.30 0.92 61.605 0.072
3 0.80 0.8 11.8 0.04760 1.4 0.0629 1.5 0.009598 0.12 0.256 78 34 61.92 0.88 61.575 0.073
4 0.71 1.1 7.3 0.04798 2.3 0.0635 2.3 0.009616 0.18 0.235 97 54 62.5 1.4 61.69 0.11
5 0.70 0.7 9.7 0.04765 1.7 0.0629 1.8 0.009595 0.14 0.236 81 41 62.0 1.1 61.559 0.085

(b) Pb* and Pbc represent radiogenic and common Pb, respectively. n.m.: Not measured (c) Corrected for fractionation, spike, and common Pb; all common Pb was assumed to be procedural blank. (d) Errors are 2σ, propagated using published algorithms51. (e) Calculations are based on published decay constants54. 206Pb/238U and 207Pb/206Pb ages corrected for initial disequilibrium in 230Th/238U using Th/U [magma] = 3.