| Baiyinnuo'er Chine | −5,36 ± 0,51 ‰ | −6,1 / −4,6 ‰ | 10 | sphalérite | Shu et al. (2013), Ore genesis and hydrothermal evolution of the Baiyinnuo'er zinc-lead s… |
| Baiyinnuo'er Chine | −5,33 ± 0,21 ‰ | −5,5 / −5,1 ‰ | 3 | galène | Shu et al. (2013), Ore genesis and hydrothermal evolution of the Baiyinnuo'er zinc-lead s… |
| Baiyinnuo'er Chine | −5,8 ± 0,42 ‰ | −6,1 / −5,5 ‰ | 2 | chalcopyrite | Shu et al. (2013), Ore genesis and hydrothermal evolution of the Baiyinnuo'er zinc-lead s… |
| Baiyinnuo'er Chine | 5,2 ‰ | | 1 | pyrite du calcaire encaissant | Shu et al. (2013), Ore genesis and hydrothermal evolution of the Baiyinnuo'er zinc-lead s… |
| District de Weibao (Weibao est et Weibao ouest) Chine | 2,45 ± 0,07 ‰ | 2,4 / 2,5 ‰ | 2 | sphalérite de Weibao est | Fang et al. (2015), Ore genesis of the Weibao lead-zinc district, Eastern Kunlun Orogen, … |
| District de Weibao (Weibao est et Weibao ouest) Chine | 1,75 ± 0,78 ‰ | 1,2 / 2,3 ‰ | 2 | galène de Weibao est | Fang et al. (2015), Ore genesis of the Weibao lead-zinc district, Eastern Kunlun Orogen, … |
| District de Weibao (Weibao est et Weibao ouest) Chine | 2,23 ± 1,95 ‰ | 0 / 3,6 ‰ | 3 | sphalérite de Weibao ouest | Fang et al. (2015), Ore genesis of the Weibao lead-zinc district, Eastern Kunlun Orogen, … |
| District de Weibao (Weibao est et Weibao ouest) Chine | −0,87 ± 0,92 ‰ | −2,2 / 0,1 ‰ | 6 | galène de Weibao ouest | Fang et al. (2015), Ore genesis of the Weibao lead-zinc district, Eastern Kunlun Orogen, … |
| District de Weibao (Weibao est et Weibao ouest) Chine | 14,97 ± 2,17 ‰ | 10,1 / 18,3 ‰ | 10 | roches encaissantes de la Formation de Langyashan | Fang et al. (2015), Ore genesis of the Weibao lead-zinc district, Eastern Kunlun Orogen, … |
| Fujigatani Japon | −7,6 ± 0,7 ‰ | −8,3 / −7 ‰ | 3 | sphalérite (corps d'Akemidani 1) | Sato (1980), Tungsten skarn deposit of the Fujigatani mine, southwest Japan, Economic Geo… |
| Fujigatani Japon | −9,3 ± 0,7 ‰ | −9,9 / −8,6 ‰ | 3 | galène (corps d'Akemidani 1) | Sato (1980), Tungsten skarn deposit of the Fujigatani mine, southwest Japan, Economic Geo… |
| Haobugao Chine | | −2,7 / −1,1 ‰ | | sulfures du minerai | Wang et al. (2019), Fluid inclusions, stable isotopes, and geochronology of the Haobugao … |
| Junosuando (champ de Masugnsbyn) Suède | | −0,8 / 1,1 ‰ | 3 | sulfures du minerai | Frietsch et al. (1995), Sulphur isotopes in Lower Proterozoic iron and sulphide ores in n… |
| Kuga (tungstène) Japon | −8 ± 1,5 ‰ | −9 / −6,9 ‰ | 2 | sphalérite | Sato (1980), Tungsten skarn deposit of the Fujigatani mine, southwest Japan, Economic Geo… |
| Kuga (tungstène) Japon | −9,7 ± 1,4 ‰ | −10,7 / −8,7 ‰ | 2 | galène | Sato (1980), Tungsten skarn deposit of the Fujigatani mine, southwest Japan, Economic Geo… |
| Lame (Lamo, champ minier de Dachang) Chine | −0,43 ‰ | | 4 | sphalérite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | 1,65 ‰ | | 2 | pyrrhotite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | −0,1 ‰ | | 1 | pyrite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | 1,2 ‰ | | 1 | arsénopyrite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | 1,8 ‰ | | 1 | chalcopyrite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | 1,8 ‰ | | 1 | jamesonite | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Lame (Lamo, champ minier de Dachang) Chine | −0,2 ‰ | | 1 | pyrite du granite de Longxianggai | Fan et al. (2004), Geochemistry and origin of tin-polymetallic sulfide deposits hosted by… |
| Nanyangtian Chine | 7,87 ± 0,29 ‰ | 7,46 / 8,07 ‰ | 4 | pyrrhotite du minerai de skarn | Zhang et al. (2021), Genesis and geodynamic setting of the Nanyangtian tungsten deposit, … |
| Nanyangtian Chine | 7,98 ‰ | | 1 | pyrite du minerai de skarn | Zhang et al. (2021), Genesis and geodynamic setting of the Nanyangtian tungsten deposit, … |
| Nanyangtian Chine | 8,86 ± 0,71 ‰ | 8,14 / 9,55 ‰ | 3 | arsénopyrite du minerai de skarn | Zhang et al. (2021), Genesis and geodynamic setting of the Nanyangtian tungsten deposit, … |
| Stora Sahavaara Suède | 0,9 ± 2,7 ‰ | −6,8 / 5,4 ‰ | 28 | pyrite et pyrrhotite du minerai et du skarn | Frietsch et al. (1995), Sulphur isotopes in Lower Proterozoic iron and sulphide ores in n… |
| Stora Sahavaara Suède | 7,3 ± 10,4 ‰ | −7,9 / 24,7 ‰ | 11 | pyrrhotite et pyrite du schiste graphiteux encaissant | Frietsch et al. (1995), Sulphur isotopes in Lower Proterozoic iron and sulphide ores in n… |
| Tervaskoski Suède | | −4,4 / 8 ‰ | | sulfures du minerai et du skarn | Frietsch et al. (1995), Sulphur isotopes in Lower Proterozoic iron and sulphide ores in n… |
| Watershed Australie | −0,5 ± 1,2 ‰ | −2,5 / 2,2 ‰ | 17 | pyrrhotite | Poblete et al. (2024), The Permian Watershed tungsten deposit (northeast Queensland, Aust… |
| Watershed Australie | 1,4 ± 1,1 ‰ | −0,2 / 2,8 ‰ | 5 | arsénopyrite | Poblete et al. (2024), The Permian Watershed tungsten deposit (northeast Queensland, Aust… |
| Watershed Australie | 0,1 ± 0,7 ‰ | −0,5 / 1,3 ‰ | 5 | pyrite et sphalérite | Poblete et al. (2024), The Permian Watershed tungsten deposit (northeast Queensland, Aust… |
| Xiaotongguanshan Chine | 3,2 ± 4,2 ‰ | −9,9 / 6 ‰ | 12 | sulfures du minerai (pyrite, pyrite colloforme, chalcopyrite) | Tian et al. (2005), REE and stable isotope geochemistry of the Xiaotongguanshan copper de… |
| Xiaotongguanshan Chine | −1 ± 4,9 ‰ | −4,4 / 2,5 ‰ | 2 | pyrite en nodules des siltites encaissantes | Tian et al. (2005), REE and stable isotope geochemistry of the Xiaotongguanshan copper de… |
| Xiaoyao Chine | 2,2 ± 0,4 ‰ | 1,8 / 2,8 ‰ | 4 | molybdénite des skarns proximaux à W-Mo | Su et al. (2026), The genesis of the Xiaoyao polymetallic tungsten deposit in the Jiangna… |
| Xiaoyao Chine | 8,7 ± 1,5 ‰ | 6,8 / 10,6 ‰ | 7 | chalcopyrite et pyrrhotite des skarns à Cu | Su et al. (2026), The genesis of the Xiaoyao polymetallic tungsten deposit in the Jiangna… |
| Xiaoyao Chine | 8,3 ± 3,3 ‰ | 6,3 / 12,1 ‰ | 3 | sphalérite des minerais distaux à Pb-Zn-Ag | Su et al. (2026), The genesis of the Xiaoyao polymetallic tungsten deposit in the Jiangna… |
| Xiaoyao Chine | 5,7 ‰ | | 1 | galène des minerais distaux à Pb-Zn-Ag | Su et al. (2026), The genesis of the Xiaoyao polymetallic tungsten deposit in the Jiangna… |
