| Banbanqiao China | 0.18 ± 0.1 ‰ | 0.07 / 0.25 ‰ | 3 | early-stage sphalerite (brown) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Banbanqiao China | 0.41 ± 0.08 ‰ | 0.36 / 0.47 ‰ | 2 | middle-stage sphalerite (red-brown) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Banbanqiao China | 0.6 ± 0.09 ‰ | 0.5 / 0.71 ‰ | 4 | late-stage sphalerite (light yellow) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Daliangzi China | −0.05 ± 0.06 ‰ | −0.11 / 0.05 ‰ | 9 | microdrilled sphalerite, specimen D-2084 (upper part of the orebody) | Zhu et al. (2020), Isotope geochemistry of Zn, Pb and S in the Ediacaran strata hosted Zn… |
| Daliangzi China | 0.1 ± 0.05 ‰ | 0.02 / 0.15 ‰ | 10 | microdrilled sphalerite, specimen D-2004 (lower part of the orebody) | Zhu et al. (2020), Isotope geochemistry of Zn, Pb and S in the Ediacaran strata hosted Zn… |
| Upper Silesia-Cracow district (Pomorzany, Chrzanów) Poland | 0.12 ± 0.19 ‰ | −0.01 / 0.26 ‰ | 2 | sphalerite | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Upper Silesia-Cracow district (Pomorzany, Chrzanów) Poland | 0.22 ‰ | | 1 | hemimorphite (Pomorzany) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Upper Silesia-Cracow district (Pomorzany, Chrzanów) Poland | 0.48 ‰ | | 1 | smithsonite (Chrzanów) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | 0.34 ‰ | | 1 | galena (Moresnet mine) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | 1.23 ± 0.22 ‰ | 0.98 / 1.39 ‰ | 3 | willemite (Moresnet, Fossey, La Calamine) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | 0.65 ± 0.29 ‰ | 0.44 / 0.85 ‰ | 2 | smithsonite (Fossey, La Calamine) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Galmoy Irlande | 0.33 ‰ | | 1 | sphalerite (CW orebody) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Galmoy Irlande | 0.41 ± 0.08 ‰ | 0.35 / 0.46 ‰ | 2 | late smithsonite (CW orebody) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Galmoy Irlande | 0.62 ± 0.63 ‰ | 0.14 / 1.33 ‰ | 3 | sphalerite (CW orebody and GY minor orebody) | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Huize China | 0.47 ± 0.08 ‰ | 0.39 / 0.64 ‰ | 10 | sphalerite of orebody No. 1 (Kuangshanchang mine) | Zhang et al. (2024), Zinc isotopes revealed the role of ore-hosting carbonate rocks in th… |
| Huize China | 0.57 ± 0.07 ‰ | 0.46 / 0.68 ‰ | 10 | sphalerite of orebody No. 10 (Qilinchang mine) | Zhang et al. (2024), Zinc isotopes revealed the role of ore-hosting carbonate rocks in th… |
| Huize China | 0.07 ± 0.19 ‰ | −0.25 / 0.34 ‰ | 11 | altered host limestones and dolostones at the ore contact | Zhang et al. (2024), Zinc isotopes revealed the role of ore-hosting carbonate rocks in th… |
| Huize China | 0.51 ± 0.15 ‰ | 0.35 / 0.71 ‰ | 6 | fresh Baizuo Formation dolostones and limestones (Sunjiagou) | Zhang et al. (2024), Zinc isotopes revealed the role of ore-hosting carbonate rocks in th… |
| Irish Midlands Zn-Pb prospects and basement veins Irlande | 0.25 ± 0.3 ‰ | 0 / 0.64 ‰ | 4 | prospect sphalerite | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Irish Midlands Zn-Pb prospects and basement veins Irlande | 0.12 ± 0.08 ‰ | 0.06 / 0.18 ‰ | 2 | sphalerite of basement feeder veins | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Jabali Yémen | 0.32 ± 0.11 ‰ | 0.24 / 0.4 ‰ | 2 | sphalerite | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Jabali Yémen | 0.6 ± 0.22 ‰ | 0.43 / 0.85 ‰ | 3 | smithsonite | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Jabali Yémen | 0.25 ‰ | | 1 | hydrozincite | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| La Florida Spain | −0.337 ± 0.342 ‰ | −0.804 / −0.003 ‰ | 6 | stage 1 sphalerite | Pašava et al. (2014), Zinc and sulfur isotope variation in sphalerite from carbonate-host… |
| La Florida Spain | 0.271 ± 0.085 ‰ | 0.211 / 0.331 ‰ | 2 | supergene hydrozincite | Pašava et al. (2014), Zinc and sulfur isotope variation in sphalerite from carbonate-host… |
| Lisheen Irlande | −0.07 ± 0.11 ‰ | −0.17 / 0.04 ‰ | 3 | sphalerite of feeder veins below the orebodies | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Lisheen Irlande | 0.233 ± 0.097 ‰ | 0.12 / 0.34 ‰ | 4 | sphalerite of orebodies (main, late and minor) | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Maoping China | 0.17 ± 0.06 ‰ | 0.08 / 0.25 ‰ | 10 | orebody I-1 sphalerite | Wu et al. (2021), Metal source and ore-forming process of the Maoping carbonate-hosted Pb… |
| Maoping China | 0.12 ± 0.11 ‰ | −0.07 / 0.25 ‰ | 13 | orebody I-2 sphalerite | Wu et al. (2021), Metal source and ore-forming process of the Maoping carbonate-hosted Pb… |
| Navan (Tara) Irlande | 0.02 ‰ | | 1 | orebody sphalerite | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Navan (Tara) Irlande | −0.09 ± 0.19 ‰ | −0.32 / 0.23 ‰ | 21 | colloform sphalerite of the 5 lens, successive microdrilled bands | Gagnevin et al. (2012), Zn, Fe and S isotope fractionation in a large hydrothermal system… |
| Navan (Tara) Irlande | 0.01 ± 0.08 ‰ | −0.08 / 0.08 ‰ | 4 | mine ore concentrates (U and 1 lenses) | Gagnevin et al. (2012), Zn, Fe and S isotope fractionation in a large hydrothermal system… |
| Navan (Tara) Irlande | 0.11 ± 0.1 ‰ | −0.02 / 0.23 ‰ | 6 | lower Palaeozoic basement rocks (altered schist, mudstones, pyroclastic rock, agglomerate, volcanogenic sediment) | Gagnevin et al. (2012), Zn, Fe and S isotope fractionation in a large hydrothermal system… |
| Niujiaotang China | −0.23 ‰ | | 1 | zinc ore (whole rock) | Xia et al. (2020), Zinc isotope revealing zinc's sources and transport processes in karst… |
| Niujiaotang China | −0.43 ± 0.02 ‰ | −0.45 / −0.42 ‰ | 2 | carbonate bedrock outside the mining area | Xia et al. (2020), Zinc isotope revealing zinc's sources and transport processes in karst… |
| Otavi Mountain Land (Berg Aukas, Baltika) Namibia | −0.06 ‰ | | 1 | sphalerite (Baltika mine) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Otavi Mountain Land (Berg Aukas, Baltika) Namibia | 0.08 ± 0.01 ‰ | 0.07 / 0.08 ‰ | 2 | willemite I (Baltika, Berg Aukas) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Otavi Mountain Land (Berg Aukas, Baltika) Namibia | −0.42 ‰ | | 1 | willemite II in veins and geodes (Berg Aukas) | Mondillo et al. (2018), A global assessment of Zn isotope fractionation in secondary Zn m… |
| Pend Oreille United States | 0.09 ‰ | | 1 | zinc concentrate (Trail smelter feed) | Shiel et al. (2010), Evaluation of zinc, cadmium and lead isotope fractionation during sm… |
| Silvermines Irlande | 0.09 ± 0.1 ‰ | 0.02 / 0.16 ‰ | 2 | sphalerite of the orebodies | Wilkinson et al. (2005), Zinc isotope variation in hydrothermal systems: preliminary evid… |
| Tianbaoshan China | 0.23 ± 0.06 ‰ | 0.14 / 0.29 ‰ | 6 | microdrilled sphalerite (specimen T8) | Zhu et al. (2020), Isotope geochemistry of Zn, Pb and S in the Ediacaran strata hosted Zn… |
| Tianqiao China | 0.1 ± 0.15 ‰ | −0.26 / 0.39 ‰ | 17 | early-stage sphalerite (brown, sphalerite-pyrite-dolomite) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Tianqiao China | 0.32 ± 0.1 ‰ | 0.18 / 0.49 ‰ | 15 | middle-stage sphalerite (brown to brown-yellow) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Tianqiao China | 0.52 ± 0.07 ‰ | 0.41 / 0.58 ‰ | 6 | late-stage sphalerite (brown-yellow to light yellow) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Tianqiao China | −0.07 ± 0.17 ‰ | −0.24 / 0.17 ‰ | 8 | Sinian to Permian sedimentary rocks (dolostones, limestones, clastic rocks) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Tianqiao China | 0.35 ± 0.08 ‰ | 0.3 / 0.44 ‰ | 3 | Emeishan basalts (Permian) | Zhou et al. (2014), Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb-Zn s… |
| Aliva Spain | 0.239 ‰ | | 1 | stage 1 sphalerite (PE-8) | Pašava et al. (2014), Zinc and sulfur isotope variation in sphalerite from carbonate-host… |
| Aliva Spain | −0.115 ± 0.27 ‰ | −0.747 / 0.081 ‰ | 8 | stage 2 sphalerite | Pašava et al. (2014), Zinc and sulfur isotope variation in sphalerite from carbonate-host… |
