Table 2
Geochemical data for the dated rocks.
Rock-type | Granite-Gneiss | Vaugnerite | Vaugnerite | Vaugnerite | Vaugnerite | |
---|---|---|---|---|---|---|
Location | Grande Roche | Clefcy quarry | Barançon quarry | Habeaurupt roadside | Tête des Sapins | |
Sample # | Vo14-16 | Vo15-01 | Vo15-04 | Vo15-07 | Vo15-08 | |
Easting (°) | 7.01681 | 6.98594 | 7.03574 | 7.01245 | 6.78311 | |
Northing (°) | 48.15902 | 48.16719 | 48.17156 | 48.14884 | 47.84628 | |
Major elements (%) by ICP-AES | ||||||
DL | ||||||
SiO2 | 0.01 | 73.06 | 48.3 | 55.46 | 58.21 | 49.27 |
Al2O3 | 0.01 | 13.36 | 9.47 | 15.48 | 16.08 | 10.86 |
Fe2O3(T) | 0.01 | 2.04 | 8.11 | 7.71 | 5.63 | 9.08 |
MnO | 0.001 | 0.02 | 0.126 | 0.11 | 0.073 | 0.161 |
MgO | 0.01 | 0.33 | 14.74 | 6.84 | 5.32 | 15.21 |
CaO | 0.01 | 0.51 | 6.44 | 5.23 | 3.38 | 8.56 |
Na2O | 0.01 | 2.57 | 1.14 | 2.68 | 2.58 | 1.15 |
K2O | 0.01 | 5.29 | 5.3 | 3.39 | 5.55 | 2.73 |
TiO2 | 0.001 | 0.232 | 1.045 | 0.876 | 0.993 | 0.519 |
P2O5 | 0.01 | 0.2 | 1.96 | 0.32 | 0.66 | 0.19 |
LOI | 0.01 | 0.76 | 2.04 | 1.33 | 1.35 | 2.72 |
Total | 98.37 | 98.69 | 99.42 | 99.82 | 100.4 | |
Trace elements (μg/g) by ICP-AES | ||||||
Sc | 1 | 4 | 20 | 17 | 15 | 37 |
Be | 1 | 3 | 7 | 4 | 8 | 2 |
V | 5 | 16 | 124 | 126 | 106 | 157 |
Ba | 3 | 364 | 1472 | 827 | 1868 | 961 |
Sr | 2 | 52 | 427 | 406 | 520 | 266 |
Y | 2 | 44 | 31 | 21 | 25 | 19 |
Zr | 4 | 153 | 315 | 223 | 448 | 131 |
Trace elements (μg/g) by ICP-MS | ||||||
Cr | 20 | <20 | 950 | 310 | 270 | 910 |
Co | 1 | 2 | 47 | 32 | 22 | 56 |
Ni | 20 | <20 | 250 | 110 | 60 | 250 |
Cu | 10 | <10 | 20 | 30 | 30 | 30 |
Zn | 30 | <30 | 70 | 80 | 70 | 50 |
Ga | 1 | 18 | 14 | 20 | 24 | 10 |
Ge | 1 | 2 | 1 | 1 | 2 | 1 |
As | 5 | <5 | 7 | <5 | 8 | 17 |
Rb | 2 | 315 | 370 | 155 | 280 | 97 |
Nb | 1 | 11 | 20 | 15 | 21 | 3 |
Mo | 2 | <2 | <2 | <2 | <2 | <2 |
Ag | 0.5 | <0.5 | <0.5 | <0.5 | 0.9 | <0.5 |
In | 0.2 | <0.2 | <0.2 | <0.2 | <0.2 | <0.2 |
Sn | 1 | 10 | 9 | 7 | 11 | 3 |
Sb | 0.5 | <0.5 | <0.5 | <0.5 | <0.5 | 1.1 |
Cs | 0.5 | 23.2 | 34.2 | 17.1 | 35.9 | 11.9 |
La | 0.1 | 23 | 53.5 | 47.3 | 72 | 20.4 |
Ce | 0.1 | 49.9 | 120 | 89.3 | 143 | 41.8 |
Pr | 0.05 | 5.7 | 16.3 | 10.2 | 16 | 4.94 |
Nd | 0.1 | 19.9 | 75.8 | 36 | 58.4 | 20.9 |
Sm | 0.1 | 4.7 | 19.3 | 6.9 | 9.7 | 4.7 |
Eu | 0.05 | 0.5 | 3.12 | 1.45 | 2.03 | 1.28 |
Gd | 0.1 | 4.8 | 11.9 | 4.8 | 6.2 | 4.6 |
Tb | 0.1 | 0.9 | 1.3 | 0.7 | 0.9 | 0.7 |
Dy | 0.1 | 6.4 | 6 | 3.9 | 4.5 | 3.7 |
Ho | 0.1 | 1.3 | 1 | 0.7 | 0.7 | 0.7 |
Er | 0.1 | 4 | 2.7 | 1.8 | 2.1 | 1.7 |
Tm | 0.05 | 0.61 | 0.34 | 0.29 | 0.32 | 0.23 |
Yb | 0.1 | 3.8 | 2.2 | 1.7 | 2 | 1.5 |
Lu | 0.04 | 0.57 | 0.33 | 0.27 | 0.32 | 0.24 |
Hf | 0.2 | 3.7 | 1.9 | 5.2 | 9.1 | 2.6 |
Ta | 0.1 | 1.7 | 1.5 | 1.4 | 2.2 | 0.1 |
W | 1 | 6 | 1 | 2 | 5 | 2 |
Tl | 0.1 | 1.7 | 4.4 | 1.3 | 1.8 | 0.9 |
Pb | 5 | 19 | 21 | 35 | 35 | 14 |
Bi | 0.4 | <0.4 | <0.4 | <0.4 | <0.4 | <0.4 |
Th | 0.1 | 16.2 | 48.7 | 19.6 | 19.1 | 12.2 |
U | 0.1 | 4.1 | 19.9 | 4.4 | 11.3 | 4.4 |
Selected parameters | ||||||
mg# | 24 | 78 | 64 | 65 | 77 | |
fn1 (Fig. 6D) | 6.85 | -0.11 | 2.40 | 0.35 | ||
fn2 (Fig. 6D) | 1.31 | 0.94 | 1.29 | 0.87 | ||
ASI | 1.28 | 0.70 | 1.21 | 1.21 | 0.86 | |
∑REE | 126 | 314 | 205 | 318 | 107 | |
Eu/Eu* | 0.32 | 0.63 | 0.77 | 0.80 | 0.84 | |
(La/Yb)N | 4 | 17 | 19 | 24 | 9 | |
Ba/Rb | 1.2 | 4.0 | 5.3 | 6.7 | 9.9 | |
Rb/Sr | 6.1 | 0.9 | 0.4 | 0.5 | 0.4 | |
Tsat Zr (°C) (1) | 801 | 641 | 758 | 844 | 606 |
DL: detection limit. LOI: loss on ignition. mg# = 100 x Mg/(Fetotal + Mg) (atomic ratios). fn1 and fn2 are composite factors computed after Scarrow et al. (2008) classification of K-rich granitoids. ASI = Al/(Na + K + 2Ca) (at.), aluminium saturation index. (./.)N denotes a ratio of values normalized to the chondrite reference of Sun and McDonough (1989). Eu/Eu* is the square root of (Eu/Gd)N x (Eu/Sm)N. (1) TSatZr are zircon saturation temperatures computed after Watson and Harrison (1983).
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