| Ashanti (Obuasi) Ghana | | 12,9 / 22,2 ‰ | | carbonates hydrothermaux des veines | Oberthur et al. 1996, Economic Geology 91:289-301 |
| Ashanti (Obuasi) Ghana | | 12,8 / 15,6 ‰ | | quartz aurifère des veines | Oberthur et al. 1996, Economic Geology 91:289-301 |
| Boliden Suède | | 10,7 / 13,5 ‰ | | minéralisation périphérique à Zn-Pb-Sb-Au (exhalative sédimentaire) | Origin of Zn-Pb-Sb-Au mineralization adjacent to the Boliden VMS, Mineralium Deposita 2017 |
| Cerro Negro (filons Marianas-San Marcos) Argentine | | −3 / 0 ‰ | | fluide hydrothermal (δ18O de l'eau) | Vidal et al. 2016, Mineralium Deposita |
| Dannemora Suède | | −1,2 / −0,4 ‰ | 5 | magnétite (Dannemora, Björnberget, Striberg) | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| District de Bafq Iran | | 0,6 / 3,4 ‰ | 6 | magnétite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| El Laco Chili | | −4,3 / 4,4 ‰ | 6 | magnétite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Gongchangling Chine | −1,32 ± 2,28 ‰ | −4 / 2,7 ‰ | 13 | magnétite du minerai riche | Wang et al. (2024), Paleoproterozoic hydrothermal overprinting over Neoarchean banded iro… |
| Gongchangling Chine | 1,8 ± 1,08 ‰ | 0,3 / 3,3 ‰ | 5 | magnétite de la BIF | Wang et al. (2024), Paleoproterozoic hydrothermal overprinting over Neoarchean banded iro… |
| Gongchangling Chine | 13,39 ± 1,29 ‰ | 10,3 / 15 ‰ | 15 | quartz de la BIF | Wang et al. (2024), Paleoproterozoic hydrothermal overprinting over Neoarchean banded iro… |
| Gongchangling Chine | 8,2 ± 1,57 ‰ | 6,5 / 9,6 ‰ | 3 | quartz du minerai riche | Wang et al. (2024), Paleoproterozoic hydrothermal overprinting over Neoarchean banded iro… |
| Grängesberg et Blötberget Suède | | −1,1 / 2,8 ‰ | 16 | magnétite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Kiirunavaara (Kiruna) Suède | | −1 / 4,1 ‰ | 14 | magnétite | Troll et al. (2019), Global Fe-O isotope correlation reveals magmatic origin of Kiruna-ty… |
| Loulo (district de Gara-Yalea) Mali | | 15,1 / 19,5 ‰ | | dolomites hydrothermales (Loulo 0, P64) | Fouillac et al. 1993, Chemical Geology |
| Massawa Sénégal | | 5,5 / 10,9 ‰ | | fluide hydrothermal (δ18O de l'eau calculé) | Treloar et al. 2015, Geological Society London Special Publications 393 |
| Matra France | 1,11 ‰ | 0,4 / 1,6 ‰ | 7 | dolomite de première génération | Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos… |
| Matra France | −3,8 ‰ | −4,4 / −3,4 ‰ | 3 | dolomite de seconde génération (MAT 2) | Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos… |
| Matra France | −0,93 ‰ | −1,1 / −0,7 ‰ | 3 | dolomite de seconde génération (MAT 32) | Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos… |
| Matra France | −2,2 ‰ | −2,8 / −1,6 ‰ | 2 | calcite (MAT 23b) | Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos… |
| Matra France | | 4,3 / 10,6 ‰ | | fluide hydrothermal (δ18O de l'eau calculé) | Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos… |
| Oyu Tolgoi Mongolie | | 8,8 / 20,1 ‰ | | alunite (sulfate) | Khashgerel et al. 2006, Economic Geology |
| Pueblo Viejo République dominicaine | | 14,6 / 19,5 ‰ | | sidérite (ciment et concrétions) | Kettler et al. 1992, Chemical Geology |