| Echo Bay (Port Radium) Canada | 22.43 ± 0.5 ‰ | 21.9 / 22.9 ‰ | 3 | stage 3 dolomite (Co-Ni arsenides) | Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo … |
| Echo Bay (Port Radium) Canada | 16.63 ± 0.68 ‰ | 16.1 / 17.4 ‰ | 3 | stage 4 calcite (early galena and chalcopyrite) | Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo … |
| Echo Bay (Port Radium) Canada | 12.88 ± 1.33 ‰ | 11.8 / 15.1 ‰ | 5 | stage 5 dolomite (main sulphides) | Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo … |
| Key Lake (Deilmann and Gaertner) Canada | 9.2 ± 1.24 ‰ | 7.1 / 11.8 ‰ | 21 | kaolinite-free Mg chlorite and illite (< 2 µm fraction) of the altered gneiss, Deilmann ore body | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 10.44 ± 2.1 ‰ | 7.6 / 13.2 ‰ | 5 | chlorite, illite and kaolinite (< 2 µm fraction) of altered gneiss from shear and ore zones, Deilmann ore body | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 11.64 ± 1.34 ‰ | 9.2 / 13.3 ‰ | 12 | illite and Mg chlorite (< 2 µm fraction) of the palaeoregolith below the unconformity, Deilmann ore body | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 8.29 ± 1.4 ‰ | 6.9 / 10.8 ‰ | 8 | chlorite and illite (< 2 µm fraction) of the altered gneiss, Gaertner ore body | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 7.8 ‰ | | 1 | fracture kaolinite in gneiss, Gaertner ore body (116GP) | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 10.5 ‰ | | 1 | vein dravite, Gaertner ore body (118GP) | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 11.79 ± 1.21 ‰ | 10.3 / 13.8 ‰ | 7 | illite (< 2 µm fraction) of the illite halo in the Athabasca sandstone above the deposit | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 14.42 ± 1.89 ‰ | 12.2 / 17.2 ‰ | 11 | kaolinite (< 2 µm fraction) of the kaolinite halo in the Athabasca sandstone | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 12.11 ± 0.74 ‰ | 10.9 / 13.1 ‰ | 9 | chlorite (< 2 µm fraction) of the sandstone chlorite zone above the deposit | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Key Lake (Deilmann and Gaertner) Canada | 9.68 ± 2.26 ‰ | 7.3 / 12.2 ‰ | 5 | Fe-Mg chlorite and kaolinite (< 2 µm fraction) of the Gaertner ore matrix | Wilson et Kyser (1987), Stable isotope geochemistry of alteration associated with the Key… |
| Zálesí Czechia | 15.56 ± 1.9 ‰ | 13.2 / 17.2 ‰ | 5 | uraninite-stage calcite | Dolníček et al. (2009), Origin of the Zálesí U–Ni–Co–As–Ag/Bi deposit, Bohemian Massif, C… |
| Zálesí Czechia | 13.5 ‰ | | 1 | arsenide-stage calcite (Za-3) | Dolníček et al. (2009), Origin of the Zálesí U–Ni–Co–As–Ag/Bi deposit, Bohemian Massif, C… |
| Zálesí Czechia | 18.05 ± 1.11 ‰ | 16.4 / 18.8 ‰ | 4 | arsenide-stage dolomite | Dolníček et al. (2009), Origin of the Zálesí U–Ni–Co–As–Ag/Bi deposit, Bohemian Massif, C… |
| Zálesí Czechia | 14.13 ± 0.96 ‰ | 13.1 / 15 ‰ | 3 | sulphide-stage calcite | Dolníček et al. (2009), Origin of the Zálesí U–Ni–Co–As–Ag/Bi deposit, Bohemian Massif, C… |
