| Batu Hijau Indonesia | | −0.48 / 0.34 ‰ | | pyrite (hydrothermal veins) | Asmoro et al. 2017, Iron-isotope systematics from the Batu Hijau Cu-Au deposit, Chemical … |
| Bayan Obo China | −0.03 ± 0.16 ‰ | | 14 | fine iron ore (bulk) | Sun et al. 2013, Iron isotopic constraints on the genesis of Bayan Obo, Precambrian Resea… |
| Bayan Obo China | 0.01 ± 0.14 ‰ | | 14 | magnetite | Sun et al. 2013, Iron isotopic constraints on the genesis of Bayan Obo, Precambrian Resea… |
| Bayan Obo China | 0.08 ± 0.18 ‰ | | 3 | hematite | Sun et al. 2013, Iron isotopic constraints on the genesis of Bayan Obo, Precambrian Resea… |
| Bayan Obo China | | −0.33 / −0.08 ‰ | | siderite (carbonatite) | Etude Fe-Mg-Sr-Nd-Pb-C-O isotopes des carbonatites a siderite de Bayan Obo, 2025 |
| Carajás Brazil | 0.25 ‰ | −0.29 / 1.02 ‰ | | hematite (martite and microplaty hematite ore) | Iron Isotopes Applied to BIF-Hosted Iron Deposits, Springer chapter (2023) |
| Carajás Brazil | | −0.3 / 0.05 ‰ | | magnetite (hydrothermally altered BIF) | Iron Isotopes Applied to BIF-Hosted Iron Deposits, Springer chapter (2023) |
| Carajás Brazil | | 0.8 / 1.1 ‰ | | martite (oxidised BIF and iron ore) | Iron Isotopes Applied to BIF-Hosted Iron Deposits, Springer chapter (2023) |
| Montagne Noire gossans France | −0.29 ± 0.04 ‰ | −0.343 / −0.238 ‰ | 4 | gossan ore (1991 experiment) | Milot et al. (2016), Iron isotopes as a potential tool for ancient iron metals tracing, J… |
| Montagne Noire gossans France | 0 ± 0.03 ‰ | −0.02 / 0.016 ‰ | 2 | gossan ore (2009 experiment) | Milot et al. (2016), Iron isotopes as a potential tool for ancient iron metals tracing, J… |
| Dannemora Sweden | | −0.57 / 0.01 ‰ | | magnetite (Dannemora, Björnberget, Striberg) | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Bafq district Iran | | 0.2 / 0.32 ‰ | 6 | magnetite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| El Laco Chile | | 0.24 / 0.36 ‰ | 6 | magnetite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Black Forest hydrothermal veins Germany | −0.91 ± 0.22 ‰ | −1.36 / −0.73 ‰ | 7 | siderite | Markl et al. (2006), Iron isotope fractionation during hydrothermal ore deposition and al… |
| Black Forest hydrothermal veins Germany | 0.06 ± 0.31 ‰ | −0.49 / 0.56 ‰ | 13 | primary hematite | Markl et al. (2006), Iron isotope fractionation during hydrothermal ore deposition and al… |
| Black Forest hydrothermal veins Germany | −0.82 ± 0.39 ‰ | −1.48 / −0.24 ‰ | 9 | secondary hematite | Markl et al. (2006), Iron isotope fractionation during hydrothermal ore deposition and al… |
| Black Forest hydrothermal veins Germany | −0.73 ± 0.23 ‰ | −1.13 / −0.51 ‰ | 6 | secondary goethite | Markl et al. (2006), Iron isotope fractionation during hydrothermal ore deposition and al… |
| Black Forest hydrothermal veins Germany | −0.23 ± 0.16 ‰ | −0.34 / 0.01 ‰ | 4 | sulfides (pyrite, chalcopyrite) | Markl et al. (2006), Iron isotope fractionation during hydrothermal ore deposition and al… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.16 ± 0.41 ‰ | −0.95 / 0.27 ‰ | 12 | quartz itabirite | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.54 ± 0.22 ‰ | −0.8 / −0.26 ‰ | 6 | massive iron ore | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.61 ‰ | | 1 | dolomitic itabirite | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.08 ± 0.67 ‰ | −0.75 / 0.83 ‰ | 4 | specularite | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | 0.03 ± 0.36 ‰ | −0.22 / 0.29 ‰ | 2 | banded iron ore | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | 0.03 ± 0.31 ‰ | −0.42 / 0.37 ‰ | 5 | schistose iron ore | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.95 ‰ | | 1 | amphibolitic itabirite | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Cauê Formation (Quadrilátero Ferrífero) Brazil | −0.22 ± 0.13 ‰ | −0.31 / −0.13 ‰ | 2 | brecciated iron ore | Mendes et al. (2017), Iron isotope and REE+Y composition of the Cauê banded iron formatio… |
| Gongchangling China | 0.82 ± 0.28 ‰ | 0.16 / 1.164 ‰ | 12 | high-grade ore magnetite | Fu et al. (2023), Fe-Si-C isotope constraints on the genesis of iron ores in Gongchanglin… |
| Gongchangling China | 0.45 ± 0.21 ‰ | 0.233 / 0.78 ‰ | 7 | BIF magnetite | Fu et al. (2023), Fe-Si-C isotope constraints on the genesis of iron ores in Gongchanglin… |
| Gongchangling China | 0.55 ± 0.03 ‰ | 0.53 / 0.57 ‰ | 2 | banded hematite ore magnetite | Fu et al. (2023), Fe-Si-C isotope constraints on the genesis of iron ores in Gongchanglin… |
| Grasberg Indonesia | | −2 / 1.1 ‰ | | sulfides (chalcopyrite and pyrite) | Graham et al. 2004, Fe isotopes in Grasberg porphyry Cu deposit |
| Grängesberg and Blötberget Sweden | | 0.11 / 0.4 ‰ | 16 | magnetite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Han-Xing China | 0.12 ± 0.03 ‰ | 0.072 / 0.207 ‰ | 15 | magnetite | Zhu et al. (2016), Iron isotope fractionation during skarn-type alteration: Implications … |
| Han-Xing China | 0.31 ± 0.14 ‰ | 0.116 / 0.482 ‰ | 7 | pyrite | Zhu et al. (2016), Iron isotope fractionation during skarn-type alteration: Implications … |
| Han-Xing China | 0.31 ± 0.03 ‰ | 0.278 / 0.353 ‰ | 5 | pyrrhotite | Zhu et al. (2016), Iron isotope fractionation during skarn-type alteration: Implications … |
| Han-Xing China | 0.08 ± 0.09 ‰ | −0.071 / 0.205 ‰ | 6 | variously altered diorites | Zhu et al. (2016), Iron isotope fractionation during skarn-type alteration: Implications … |
| Isua (BIF) Greenland | | 0.1 / 0.5 ‰ | | magnetite | Dauphas et al. 2004, Fe isotopes in Isua BIF |
| Jiaojia (Jiaodong gold district) China | 0.1 ± 0.09 ‰ | 0.07 / 0.62 ‰ | 40 | disseminated pyrite | Zhu et al. (2018), Iron isotope behavior during fluid/rock interaction in K-feldspar alte… |
| Jinchuan China | −0.66 ± 0.34 ‰ | −0.9 / −0.16 ‰ | 4 | pyrrhotite | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Jinchuan China | 0.87 ± 0.29 ‰ | 0.53 / 1.05 ‰ | 3 | pentlandite | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Jinchuan China | 0.33 ± 0.25 ‰ | 0.15 / 0.5 ‰ | 2 | chalcopyrite | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Jinchuan China | 0.48 ± 0.24 ‰ | 0.24 / 0.71 ‰ | 3 | magnetite | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Jinchuan China | 0.56 ± 0.06 ‰ | 0.52 / 0.6 ‰ | 2 | serpentine | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Jinchuan China | 0.05 ± 0.02 ‰ | 0.04 / 0.07 ‰ | 3 | primary silicates (olivine, clinopyroxene, orthopyroxene) | Wang et al. (2021), Iron Isotope Compositions of Coexisting Sulfide and Silicate Minerals… |
| Kiirunavaara (Kiruna) Sweden | | 0.12 / 0.41 ‰ | 11 | magnetite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Linglong (Jiaodong gold district) China | −0.07 ± 0.35 ‰ | −1.01 / 0.76 ‰ | 24 | quartz-vein pyrite | Zhu et al. (2018), Iron isotope behavior during fluid/rock interaction in K-feldspar alte… |
| Datangpo-type manganese (Gaolou, Minle, Zhenxing) China | −0.49 ± 0.14 ‰ | −0.73 / −0.32 ‰ | 9 | manganese ore, whole rock (Gaolou) | He et al. (2024), Redox conditions of Datangpo-type manganese ores constrained by statist… |
| Datangpo-type manganese (Gaolou, Minle, Zhenxing) China | −0.06 ± 0.45 ‰ | −0.71 / 0.48 ‰ | 6 | host mudstones, whole rock (Gaolou) | He et al. (2024), Redox conditions of Datangpo-type manganese ores constrained by statist… |
| Datangpo-type manganese (Gaolou, Minle, Zhenxing) China | 0.28 ± 0.13 ‰ | 0.12 / 0.54 ‰ | 12 | pyrite (Minle) | He et al. (2024), Redox conditions of Datangpo-type manganese ores constrained by statist… |
| Datangpo-type manganese (Gaolou, Minle, Zhenxing) China | 0.37 ± 0.22 ‰ | 0.03 / 0.67 ‰ | 10 | pyrite (Zhenxing) | He et al. (2024), Redox conditions of Datangpo-type manganese ores constrained by statist… |
| Eyller Bruch bog iron ore Germany | −0.19 ± 0.14 ‰ | −0.39 / 0.03 ‰ | 7 | nodules and clays (Tote Rahm) | Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron … |
| Eyller Bruch bog iron ore Germany | −0.55 ± 0.35 ‰ | −1.29 / −0.09 ‰ | 11 | nodules and crusts (Gelderner Fleuth) | Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron … |
| Eyller Bruch bog iron ore Germany | 0.36 ± 0.49 ‰ | 0.03 / 1.16 ‰ | 5 | ore used for an experimental smelt | Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron … |
| Lahn-Dill ores (Grube Fortuna, Wetzlar) Germany | 0.56 ± 0.05 ‰ | 0.51 / 0.62 ‰ | 6 | hematite (Grube Fortuna) | Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron … |
| Lahn-Dill ores (Grube Fortuna, Wetzlar) Germany | 0.73 ± 0.21 ‰ | 0.49 / 1 ‰ | 4 | hematite (ore heap near Wetzlar) | Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron … |
| Zankan China | 0.2 ± 0.34 ‰ | −0.3 / 0.5 ‰ | 5 | magnetite | Zhou et al. (2017), Trace elements of magnetite and iron isotopes of the Zankan iron depo… |
| Zankan China | 0.7 ± 0.12 ‰ | 0.6 / 0.8 ‰ | 4 | pyrite | Zhou et al. (2017), Trace elements of magnetite and iron isotopes of the Zankan iron depo… |