Escanaba Trough hydrothermal fluids (Gorda Ridge)
Escanaba Trough
Other media
- Type
- Other medium
Seafloor hydrothermal fluids compiled and measured by Palmer (1991). Coordinates not published. Clastic sediment-covered system (water/rock ratio about 5 from alkalis).
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 10.7 ± 0.7 ‰ | 10.1 / 11.5 ‰ | 3 | seafloor hydrothermal fluid (dissolved boron) Mean and standard deviation recalculated from 3 analyses, +10.1 to +11.5 (2040 +11.5; 2036 +10.1; 2041 +10.4). 1.71 to 2.16 mmol/kg B; lowest values of the seafloor fluids. Uncertainty of 2040 illegible in the source. | Palmer (1991), Boron isotope systematics of hydrothermal fluids and tourmalines: A synthe… |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Escanaba Trough hydrothermal fluids (Gorda Ridge), isotope signatures. https://www.isofind.tech/isotopes/en/sites/fluides-hydrothermaux-de-la-fosse-d-escanaba-dorsale-de-gorda/ (accessed 2026-10-19).
@misc{isofind2026escanabatroughhydrothermalflu,
title = {Escanaba Trough hydrothermal fluids (Gorda Ridge), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/fluides-hydrothermaux-de-la-fosse-d-escanaba-dorsale-de-gorda/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19