| Bingham Canyon United States | −4.15 ± 3.25 ε | −8.8 / −1.3 ε | 4 | altered intrusive rocks (latite porphyry, lamprophyre, monzonite; whole rock) | Fitzpayne et al. (2018), Assessing Thallium Elemental Systematics and Isotope Ratio Varia… |
| Bingham Canyon United States | −2.03 ± 1.95 ε | −4.2 / 0.9 ε | 7 | unbrecciated sedimentary host rocks (sandstones, silicified limestones, quartzites; whole rock) | Fitzpayne et al. (2018), Assessing Thallium Elemental Systematics and Isotope Ratio Varia… |
| Bingham Canyon United States | 2.07 ± 4.8 ε | −2.3 / 7.2 ε | 3 | hydrothermal breccias (silicified limestone, quartzites; whole rock) | Fitzpayne et al. (2018), Assessing Thallium Elemental Systematics and Isotope Ratio Varia… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | 0.8 ± 1.98 ε | −0.6 / 2.2 ε | 2 | igneous K-feldspar of unaltered granodiorite | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −1.53 ± 1.72 ε | −2.9 / 0.4 ε | 3 | igneous mica (phlogopite, annite) of unaltered granodiorite | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −2.76 ± 1.37 ε | −5 / −1.6 ε | 5 | K-feldspar from weak potassic alteration | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −3.85 ± 0.68 ε | −4.8 / −3.2 ε | 4 | mica (phlogopite, annite) from weak potassic alteration | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −3.57 ± 0.8 ε | −5 / −2.4 ε | 9 | K-feldspar from strong potassic alteration (rock and veinlets) | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −4.4 ± 0.4 ε | | 1 | phlogopite from strong potassic alteration | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −1.76 ± 0.87 ε | −3.1 / −0.8 ε | 5 | K-feldspar from sodic-calcic alteration (rock and veinlets) | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
| Battle Mountain district (Copper Basin, Elder Creek) United States | −2.8 ± 2.12 ε | −4.3 / −1.3 ε | 2 | mica (annite, phlogopite) from sodic-calcic alteration | Rader et al. (2023), New constraints on fluid chemistry and elemental mobility during hyd… |
