Semi glacier water (Tibet)
Southern Tibet (Xizang), Shiquanhe-Yarlung Zangbo geothermal field, China
Other media
- Type
- Other medium
Glacier water from the Semi area; high-mountain glaciers are the main water source of the geothermal springs according to H-O isotopes (Tan et al., 2014). Coordinates not published.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −8.4 ‰ | 1 | glacial meltwater (dissolved boron) Single analysis (SM-7). 2.7 mg/L HBO2; uncertainty 0.7 ‰. | Li et al. (2023), Boron isotope constraints on the migration and accumulation of rare alk… |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Semi glacier water (Tibet), isotope signatures. https://www.isofind.tech/isotopes/en/sites/eau-de-glacier-de-semi-tibet/ (accessed 2026-10-19).
@misc{isofind2026semiglacierwatertibetisotopes,
title = {Semi glacier water (Tibet), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/eau-de-glacier-de-semi-tibet/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19