Hot brines of the Suakin and Valdivia deeps (Red Sea)
Red Sea
Other media
- Type
- Other medium
Seafloor hydrothermal fluids compiled and measured by Palmer (1991). Coordinates not published. Deep brines fed by marine evaporites.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 34.6 ± 6.2 ‰ | 30.2 / 39 ‰ | 2 | seafloor hydrothermal fluid (dissolved boron) Mean and standard deviation recalculated from 2 analyses, +30.2 to +39.0 (Suakin +39.0; Valdivia +30.2). 0.63 and 0.80 mmol/kg B. | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Hot brines of the Suakin and Valdivia deeps (Red Sea), isotope signatures. https://www.isofind.tech/isotopes/en/sites/saumures-chaudes-des-fosses-suakin-et-valdivia-mer-rouge/ (accessed 2026-10-19).
@misc{isofind2026hotbrinesofthesuakinandvaldiv,
title = {Hot brines of the Suakin and Valdivia deeps (Red Sea), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/saumures-chaudes-des-fosses-suakin-et-valdivia-mer-rouge/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19