Hydrothermal fluids of the East Pacific Rise at 11-13° N
East Pacific Rise
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- Type
- Other medium
Seafloor hydrothermal fluids compiled and measured by Palmer (1991). Coordinates not published. Sediment-starved fast-spreading ridge.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 34.9 ± 2 ‰ | 31.7 / 36.8 ‰ | 5 | seafloor hydrothermal fluid (dissolved boron) Mean and standard deviation recalculated from 5 analyses, +31.7 to +36.8 (1 +34.9; 3 +36.8; 4 +31.7; 5 +36.6; 6 +34.7). 0.45 to 0.49 mmol/kg B. Values of Spivack and Edmond (1987). | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Hydrothermal fluids of the East Pacific Rise at 11-13° N, isotope signatures. https://www.isofind.tech/isotopes/en/sites/fluides-hydrothermaux-de-la-dorsale-est-pacifique-a-11-13-n/ (accessed 2026-10-19).
@misc{isofind2026hydrothermalfluidsoftheeastpa,
title = {Hydrothermal fluids of the East Pacific Rise at 11-13° N, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/fluides-hydrothermaux-de-la-dorsale-est-pacifique-a-11-13-n/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19