| Lac Da Qaidam : fossé de Datoo Yong (point 20) Chine | 8,61 ‰ | | 1 | eau de surface (bore dissous) | Xiao et al. (1992), Boron isotopic compositions of brine, sediments, and source water in … |
| Lac de Zabuye : rivière (W1) Chine | −10,51 ‰ | | 1 | eau de rivière (bore dissous) | Zhang et al. (2023), Boron source and evolution of the Zabuye salt lake, Tibet: Indicatio… |
| Rivière Bai Kok (bassin de Lakkor Co) Chine | −14,7 ± 1,32 ‰ | −15,63 / −13,76 ‰ | 2 | eau de rivière (bore dissous) | Li et al. (2022), Boron isotope geochemistry of the Lakkor Co salt lake (Tibet) and its g… |
| Rivière Daqu (bassin de Bangor Co) Chine | −0,52 ‰ | | 1 | eau de rivière (bore dissous) | Li et al. (2022), Boron isotope geochemistry of Bangor Co Salt Lake (central Tibet): impl… |
| Rivière Graza (bassin de Bangor Co) Chine | 3,78 ± 1,2 ‰ | 2,93 / 4,62 ‰ | 2 | eau de rivière (bore dissous) | Li et al. (2022), Boron isotope geochemistry of Bangor Co Salt Lake (central Tibet): impl… |
| Rivière Nalenggele (bassin du Qaidam) Chine | −2,42 ‰ | | 1 | eau de rivière (bore dissous) | Wei et al. (2014), Boron isotope geochemistry of salt sediments from the Dongtai salt lak… |
| Rivière Somme (bassin de Lakkor Co) Chine | −10,56 ± 0,83 ‰ | −11,15 / −9,97 ‰ | 2 | eau de rivière (bore dissous) | Li et al. (2022), Boron isotope geochemistry of the Lakkor Co salt lake (Tibet) and its g… |
| Rivières de Basse-Terre mêlées de sources thermales (Carbet, Galion) France | 20,6 ± 6,1 ‰ | 12,1 / 25,3 ‰ | 4 | eau de rivière (bore dissous) | Louvat et al. (2011), Boron isotope ratios of surface waters in Guadeloupe, Lesser Antill… |
| Rivières de Basse-Terre sans apport hydrothermal (Guadeloupe) France | 42,5 ± 2 ‰ | 39,1 / 44,8 ‰ | 11 | eau de rivière (bore dissous) | Louvat et al. (2011), Boron isotope ratios of surface waters in Guadeloupe, Lesser Antill… |
| Ruisseau de Dagejia (Changmaqu, Tibet) Chine | −14,5 ± 0,4 ‰ | −15 / −14 ‰ | 4 | eau de ruisseau (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
| Ruisseaux de Semi (Tibet) Chine | −10,9 ± 0,5 ‰ | −11,5 / −10,5 ‰ | 3 | eau de ruisseau (bore dissous) | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
