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ODP Hole 1026B, eastern flank of the Juan de Fuca Ridge (low-temperature fluid)

Juan de Fuca Ridge, northeast Pacific

Groundwater

Type
Groundwater

Warm fluid (50 to 60 C) from 3.5 Ma basaltic basement, sampled from the casing of ODP Hole 1026B (Leg 168) two years after drilling (Sharma et al., 2000). Coordinates not published.

187Os/188Os isotope ratio, no unit Values of the same system

Standard : Rapport absolu, sans standard de référence

ValueRangenMineral or matrixSource
0.111low-temperature basement fluid
Single analysis (ODP 1026B). ODP 1026B: 50 °C, Mg 2.42 mmol/kg, Cl 555 (556) mmol/kg, Os 518 fmol/kg, measured 0.111, corrected 0.11 ± 0.001. Cl in brackets: content corrected for seawater contamination during sampling. Os 518 fmol/kg and 187Os/188Os 0.110, below MORB (about 0.125): sign of an anciently depleted mantle domain beneath the ridge according to the authors.
Sharma et al. (2000), Osmium isotopes in hydrothermal fluids from the Juan de Fuca Ridge,…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). ODP Hole 1026B, eastern flank of the Juan de Fuca Ridge (low-temperature fluid), isotope signatures. https://www.isofind.tech/isotopes/en/sites/forage-odp-1026b-flanc-est-de-la-dorsale-juan-de-fuca-fluide-de-basse-temperature/ (accessed 2026-10-21).

@misc{isofind2026odphole1026beasternflankofthe,
  title = {ODP Hole 1026B, eastern flank of the Juan de Fuca Ridge (low-temperature fluid), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/forage-odp-1026b-flanc-est-de-la-dorsale-juan-de-fuca-fluide-de-basse-temperature/},
  note = {Accessed 2026-10-21}
}

Updated : 2026-10-21