Get Essential, free

Echo Bay (Port Radium)

Northwest Territories, east shore of Great Bear Lake, Canada

UraniumAg-U-Cu (Ni, Co, Bi)

Type
U-Ni-Ag-Cu veins (five-element association)

Veins along NE-SW fractures in about 1800 Ma andesitic tuffs (Cliff Series), adjacent to the old Eldorado mine at Port Radium; 1971 production of about 75 t silver and 300 t copper. Seven stages: quartz-hematite, pitchblende, Co-Ni arsenides with native silver and bismuth, early acanthite, main sulphide and dolomite, late native silver, mckinstryite. About 120 °C (stages 1 to 4), 200 °C (stages 5 and 6), below 95 °C (stage 7), at 2.5 to 4.5 km depth; halite-bearing inclusions with about 30 wt% salts. Fluid at δ18O +1.0 ± 2.5 ‰, δ34S ΣS +25 ± 3 ‰ and δ13C ΣC -5 ± 2 ‰: seawater circulating and boiling around a diabase at about 1450 Ma according to the authors; sulphide δ34S from -22 ‰ (early acanthite) to +27 ‰ (mckinstryite), through a progressive decrease of the fluid oxidation state. Coordinates from the authors.

δ18O in ‰ (per mil) Values of the same system

Standard : V-SMOW

ValueRangenMineral or matrixSource
22.43 ± 0.5 ‰21.9 / 22.9 ‰3stage 3 dolomite (Co-Ni arsenides)
Mean and standard deviation recalculated from 3 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
16.63 ± 0.68 ‰16.1 / 17.4 ‰3stage 4 calcite (early galena and chalcopyrite)
Mean and standard deviation recalculated from 3 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
12.88 ± 1.33 ‰11.8 / 15.1 ‰5stage 5 dolomite (main sulphides)
Mean and standard deviation recalculated from 5 analyses, fluid δ18O near +1 ‰ at about 200 °C according to the authors.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …

δ13C in ‰ (per mil) Values of the same system

Standard : V-PDB

ValueRangenMineral or matrixSource
−3.23 ± 0.75 ‰−4.1 / −2.8 ‰3stage 3 dolomite (Co-Ni arsenides)
Mean and standard deviation recalculated from 3 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
−3.17 ± 0.81 ‰−3.9 / −2.3 ‰3stage 4 calcite (early galena and chalcopyrite)
Mean and standard deviation recalculated from 3 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
−2.08 ± 0.65 ‰−3 / −1.4 ‰5stage 5 dolomite (main sulphides)
Mean and standard deviation recalculated from 5 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …

δ34S in ‰ (per mil) Values of the same system

Standard : V-CDT

ValueRangenMineral or matrixSource
3.95 ± 1.05 ‰2.4 / 5.1 ‰6pyrite of host tuffs (over 200 m from veins)
Mean and standard deviation recalculated from 6 analyses, values typical of igneous-rock sulphur.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
2.15 ± 0.07 ‰2.1 / 2.2 ‰2pyrite of hornblende-magnetite veins
Mean and standard deviation recalculated from 2 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
−20.6 ± 1.27 ‰−21.5 / −19.7 ‰2stage 4 acanthite
Mean and standard deviation recalculated from 2 analyses, the earliest and lightest sulphides.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
−0.83 ± 1.2 ‰−2 / 0.4 ‰3stage 4 colloform marcasite
Mean and standard deviation recalculated from 3 analyses, S30 analysed twice (-2.0 ‰).
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
−2.3 ± 2.55 ‰−4.1 / −0.5 ‰2stage 5 acanthite (with carbonates)
Mean and standard deviation recalculated from 2 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
9.5 ± 7.5 ‰2.5 / 19.9 ‰4stage 5 galena
Mean and standard deviation recalculated from 4 analyses, S18 averaged over two analyses (+2.4 and +2.6 ‰).
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
8.06 ± 4.02 ‰4.1 / 12.55 ‰4stage 5 sphalerite
Mean and standard deviation recalculated from 4 analyses, S36 averaged over two analyses (+12.5 and +12.6 ‰); sphalerite-galena pairs at 245 ± 35 and 220 ± 30 °C.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
6.86 ± 3.26 ‰3.7 / 13.5 ‰7stage 5 chalcopyrite
Mean and standard deviation recalculated from 7 analyses.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
7.9 ± 4.49 ‰5.1 / 14.6 ‰4stage 5 bornite
Mean and standard deviation recalculated from 4 analyses, S43 (+14.6 ‰) associated with late chalcopyrite.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
21.3 ‰1stage 6 acanthite (S27)
Single analysis.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …
24.4 ± 1.78 ‰23 / 27 ‰4stage 7 mckinstryite
Mean and standard deviation recalculated from 4 analyses, S41 averaged over two analyses (+26.9 and +27.1 ‰); the latest and heaviest sulphides.
Robinson et Ohmoto (1973), Mineralogy, Fluid Inclusions, and Stable Isotopes of the Echo …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Echo Bay (Port Radium), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/echo-bay-port-radium/ (accessed 2026-10-14).

@misc{isofind2026echobayportradiumisotopesigna,
  title = {Echo Bay (Port Radium), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/echo-bay-port-radium/},
  note = {Accessed 2026-10-14}
}

Updated : 2026-10-14