| Autres sources chaudes de Java (Ciawi, Cipanas, Kalianget) Indonésie | 4,26 ± 4,81 ‰ | −0,7 / 8,9 ‰ | 3 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal d'El Tatio (Chili) Chili | −4,6 ‰ | | 1 | eau de source chaude (bore dissous) | Schmitt et al. (2002), Boron in central Andean ignimbrites: implications for crustal boro… |
| Champ géothermal de Chabu (Tibet) Chine | −16,52 ± 0,08 ‰ | −16,57 / −16,46 ‰ | 2 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Champ géothermal de Chabu (Tibet) Chine | −16,57 ‰ | | 1 | eau géothermale de Chabu (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Champ géothermal de Dieng (Java) Indonésie | 2,7 ± 2,22 ‰ | 0,27 / 4,62 ‰ | 3 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Dieng (Java) Indonésie | 34,86 ‰ | | 1 | eau de lac de cratère acide sulfaté (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Dieng (Java) Indonésie | 0,12 ± 0,2 ‰ | −0,02 / 0,26 ‰ | 2 | saumure géothermale de forage (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Kamojang (Java) Indonésie | 2,3 ‰ | | 1 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Kamojang (Java) Indonésie | 9,27 ‰ | | 1 | eau de lac de cratère acide sulfaté (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Kamojang (Java) Indonésie | 3,84 ‰ | | 1 | condensat de vapeur d'évent (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Champ géothermal de Puga (Ladakh) Inde | −12,7 ± 0,3 ‰ | −13,1 / −12,2 ‰ | 6 | fluide géothermal de source chaude (bore dissous) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −12,8 ‰ | | 1 | eau interstitielle d'une mare de boue (filtrée) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −14,4 ± 0,1 ‰ | −14,5 / −14,3 ‰ | 2 | croûtes et pâtes évaporitiques (halite, tincalconite) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −17,6 ‰ | | 1 | sédiment de bordure de mare de boue (muscovite, soufre) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −36 ± 2,6 ‰ | −37,8 / −34,1 ‰ | 2 | fritte siliceuse (croûte laminée et nodules digités de silice amorphe) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −28,3 ‰ | | 1 | sédiment de source chaude (quartz, muscovite, calcite) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Puga (Ladakh) Inde | −41 ‰ | | 1 | sédiment en suspension riche en diatomées (mare de boue) | Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp… |
| Champ géothermal de Yangbajing (Tibet) Chine | −11,64 ± 2,89 ‰ | −13,83 / −8,37 ‰ | 3 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Champ géothermal de Yangbajing (Tibet) Chine | −12,73 ‰ | | 1 | eau géothermale de Yangbajing (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Eau de glacier de Semi (Tibet) Chine | −8,4 ‰ | | 1 | eau de fonte glaciaire (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
| Eaux évaporées des volcans de boue de Kertch (Korolevsky, Central Lake Hill) Crimée | 9,8 ± 2,1 ‰ | 8,3 / 11,3 ‰ | 2 | eau (bore dissous) | Lin et al. (2026), Application of boron isotopes to the understanding of fluid-rock inter… |
| Fluides hydrothermaux de la dorsale Est-Pacifique à 11-13° N | 34,9 ± 2 ‰ | 31,7 / 36,8 ‰ | 5 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux de la dorsale Est-Pacifique à 21° N | 31,4 ± 1,4 ‰ | 29 / 32,7 ‰ | 8 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux de la fosse d'Escanaba (dorsale de Gorda) | 10,7 ± 0,7 ‰ | 10,1 / 11,5 ‰ | 3 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux de la fosse des Mariannes (bassin d'arrière-arc) | 26,1 ± 3,7 ‰ | 22,5 / 29,8 ‰ | 3 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux du bassin de Guaymas (golfe de Californie) | 19,2 ± 3 ‰ | 16,5 / 23,2 ‰ | 4 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux du monticule actif de TAG (dorsale médio-atlantique) | 30,7 ± 2,3 ‰ | 29,1 / 32,3 ‰ | 2 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Fluides hydrothermaux du site MARK (dorsale médio-atlantique, 23° N) | 26,8 ± 0,1 ‰ | 26,7 / 26,9 ‰ | 2 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Grands volcans de boue profonds de Kertch (Big Tarkhan, Andrusov, Oldenburgsky) Crimée | 12,3 ± 1,4 ‰ | 10,7 / 13,6 ‰ | 6 | eau (bore dissous) | Lin et al. (2026), Application of boron isotopes to the understanding of fluid-rock inter… |
| Lac Da Qaidam : pluie Chine | 16,69 ‰ | | 1 | pluie (bore dissous) | Xiao et al. (1992), Boron isotopic compositions of brine, sediments, and source water in … |
| Lac Siling Co (Tibet) Chine | 0,1 ‰ | | 1 | eau de lac salé (bore dissous) | Li et al. (2022), Boron isotope geochemistry of Bangor Co Salt Lake (central Tibet): impl… |
| Lac de Zabuye : marais (W3) Chine | −8,82 ‰ | | 1 | eau de marais (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Lac de cratère de Kawah Putih (volcan Patuha, Java) Indonésie | 0,59 ‰ | | 1 | eau de lac de cratère acide chloruré (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Lacs d'eau douce de Ganga Co et Ziza Co (bassin de Lakkor Co) Chine | −15,2 ± 0,4 ‰ | −15,48 / −14,91 ‰ | 2 | eau de lac (bore dissous) | Li et al. (2022), Boron isotope geochemistry of the Lakkor Co salt lake (Tibet) and its g… |
| Panache hydrothermal de la dorsale Juan de Fuca | 34,5 ‰ | | 1 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Petits volcans de boue peu profonds de Kertch (Tobichek, Eny-Kale, Soldatsko-Slobodsky) Crimée | 37,7 ± 18,1 ‰ | 18,6 / 54,7 ‰ | 3 | eau (bore dissous) | Lin et al. (2026), Application of boron isotopes to the understanding of fluid-rock inter… |
| Salars de l'Altiplano chilien (Aguas Calientes, Sico, Tuyaito) Chili | 2 ± 4,3 ‰ | −2,7 / 5,7 ‰ | 3 | eau de salar (bore dissous) | Schmitt et al. (2002), Boron in central Andean ignimbrites: implications for crustal boro… |
| Salars de la Puna occidentale (Arizaro, Río Grande, Antofalla) Argentine | −5 ± 1,2 ‰ | −6,6 / −3,7 ‰ | 4 | saumure de salar (bore dissous) | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Salars de la Puna occidentale (Arizaro, Río Grande, Antofalla) Argentine | −5,9 ± 8,4 ‰ | −14,6 / 5,2 ‰ | 6 | halite de salar | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Salinas Grandes (Puna orientale) Argentine | −18,3 ‰ | | 1 | saumure de salar (bore dissous) | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Salinas Grandes (Puna orientale) Argentine | −14,5 ‰ | | 1 | halite de salar | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Saumures chaudes des fosses Suakin et Valdivia (mer Rouge) | 34,6 ± 6,2 ‰ | 30,2 / 39 ‰ | 2 | fluide hydrothermal de fond de mer (bore dissous) | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
| Source chaude de Kawu (Tibet) Chine | −12,56 ‰ | | 1 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Source chaude de Kawu (Tibet) Chine | −11,7 ± 0,6 ‰ | −12,1 / −11,2 ‰ | 2 | eau géothermale (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
| Source chaude de Zhegu (Tibet méridional) Chine | 0,52 ‰ | | 1 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Source thermale d'Antuco (Puna) Argentine | −12,5 ‰ | | 1 | eau thermale (bore dissous) | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Source thermale de Botijuela (Puna occidentale) Argentine | 0,7 ‰ | | 1 | eau thermale (bore dissous) | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Sources chaudes côtières à apport d'eau de mer (Parangtritis, Krakal, Java) Indonésie | 26,77 ± 2,73 ‰ | 24,84 / 28,7 ‰ | 2 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources chaudes de Dagejia (Tibet) Chine | −15,7 ± 0,3 ‰ | −15,9 / −15,4 ‰ | 3 | eau géothermale (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
| Sources chaudes de Semi (Tibet) Chine | −19,6 ± 1,3 ‰ | −21,2 / −18,3 ‰ | 4 | eau géothermale (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
| Sources chaudes de Semi (Tibet) Chine | −12,46 ‰ | | 1 | eau géothermale de Semi (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Sources chaudes de volcans quaternaires de Java (Lamongan, Tampomas, Pangalengan, Darajat) Indonésie | 4,73 ± 6,33 ‰ | −0,95 / 12,81 ‰ | 4 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources chaudes des systèmes de faille de Java (Batu Kapur, Pakenjeng, Cilayu, Cikundul, Cisolok) Indonésie | 1,3 ± 4,59 ‰ | −2,36 / 9,31 ‰ | 5 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources chaudes du complexe Arjuna-Welirang (Java) Indonésie | 9,55 ± 3,44 ‰ | 7,12 / 11,98 ‰ | 2 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources chaudes du volcan Lawu (Java) Indonésie | 4,64 ± 3,37 ‰ | 1,33 / 8,07 ‰ | 3 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources chaudes du volcan Slamet (Java) Indonésie | 6,84 ± 1,32 ‰ | 5,9 / 7,77 ‰ | 2 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Sources géothermales de Gulu et Qucai (rift de Yadong-Gulu, Tibet) Chine | −6,45 ± 0,86 ‰ | −7,06 / −5,84 ‰ | 2 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Sources géothermales à bore faible du bloc de Lhasa (Xiqin, Qiaga, Xizha, Caizha, Xueru, Ruduo, Dezhong) Chine | −10,99 ± 3,29 ‰ | −13,61 / −5,96 ‰ | 7 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Sources géothermales à bore faible du bloc de Lhasa (Xiqin, Qiaga, Xizha, Caizha, Xueru, Ruduo, Dezhong) Chine | −12,82 ‰ | | 1 | eau géothermale de Caizha (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Sources géothermales à bore élevé du Tibet méridional (Buxionglanggu, Shagalangga, Babudemi, Chaka, Lawangzi) Chine | −11,27 ± 0,65 ‰ | −12,43 / −10,87 ‰ | 5 | eau géothermale (bore dissous) | Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O… |
| Sources thermales actives de la Puna orientale (Tuzgle, Baños de Pompeya, Baños Incachule, Puente del Diablo, Luracatao) Argentine | −12,8 ± 1,8 ‰ | −15,3 / −10,4 ‰ | 5 | eau thermale (bore dissous) | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Sources thermales actives de la Puna orientale (Tuzgle, Baños de Pompeya, Baños Incachule, Puente del Diablo, Luracatao) Argentine | −9,3 ± 6,2 ‰ | −16,4 / −5,2 ‰ | 3 | halite de source thermale | Kasemann et al. (2004), Boron isotope composition of geothermal fluids and borate mineral… |
| Sources thermales de la Soufrière (Guadeloupe) France | 11,7 ± 2,8 ‰ | 8,1 / 15,1 ‰ | 5 | eau thermale (bore dissous) | Louvat et al. (2011), Boron isotope ratios of surface waters in Guadeloupe, Lesser Antill… |
| Sources thermales de la Soufrière (Guadeloupe) France | 12 ‰ | | 1 | eau de source (bore dissous) | Louvat et al. (2011), Boron isotope ratios of surface waters in Guadeloupe, Lesser Antill… |
| Suévite de cratère du Ries, forage Nördlingen 1973 Allemagne | −4,1 ± 4,2 ‰ | −8,9 / −1,2 ‰ | 3 | smectite secondaire (< 2 µm) | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Suévite de cratère du Ries, forage Nördlingen 1973 Allemagne | −21,8 ‰ | | 1 | smectite secondaire (< 2 µm), base du forage | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Suévite de retombée du Ries à Amerdingen Allemagne | −23,6 ‰ | | 1 | smectite secondaire (< 2 µm) | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Suévite de retombée du Ries à Aumühle Allemagne | −26,3 ‰ | | 1 | smectite secondaire (< 2 µm) | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Suévite de retombée du Ries à Lehberg Allemagne | −22,7 ‰ | | 1 | smectite secondaire (< 2 µm) | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Suévite de retombée du Ries à Otting Allemagne | −25,6 ‰ | | 1 | smectite secondaire (< 2 µm) | Muttik et al. (2011), Boron isotope composition of secondary smectite in suevites at the … |
| Taruo Co (lac et rivière) Chine | −4,84 ‰ | | 1 | eau de rivière (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Taruo Co (lac et rivière) Chine | −10,32 ‰ | | 1 | eau du lac (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Volcan Tangkuban Parahu (Java) Indonésie | 2,4 ‰ | | 1 | eau de source chaude (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
| Volcan Tangkuban Parahu (Java) Indonésie | 5,54 ‰ | | 1 | eau de lac de cratère acide sulfaté (bore dissous) | Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,… |
