Salton Sea Geothermal Field
California (Imperial Valley), United States
Geothermal brinesLi
- Type
- Geothermal brine
δ7Li of 3.7 to 4.7 ‰ (McKibben, 2024). The brine is very homogeneous, controlled by temperature and chlorite. The lithium resource is under development (EnergySource Minerals).
δ7Li in ‰ (per mil) Values of the same system
Standard : L-SVEC
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 4.2 ‰ | 3.7 / 4.7 ‰ | 20 | Characterization of Li in the Salton Sea Geothermal Field (2024) |
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 12 ‰ | Characterization of Li in the Salton Sea Geothermal Field (2024) |
Cite this page
IsoFind Atlas (2026). Salton Sea Geothermal Field, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/salton-sea-geothermal-field/ (accessed 2026-10-06).
@misc{isofind2026saltonseageothermalfieldisoto,
title = {Salton Sea Geothermal Field, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/salton-sea-geothermal-field/},
note = {Accessed 2026-10-06}
}Updated : 2026-10-06