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Eagle Point (Athabasca)

Saskatchewan, eastern margin of the Athabasca Basin (Rabbit Lake area), Canada

UraniumU

Type
Basement-hosted Proterozoic unconformity uranium

Uranium ore sample from the Queen's University collection analysed by Uvarova et al. (2014) for δ238U and δ234U. Basement-hosted deposit with its extension (Eagle Point Extension) (Cloutier et al., 2011): primary and remobilised uraninite, secondary becquerelite; δ238U of +0.37 to +0.90 ‰ and δ234U of -217 to +281 ‰, the most scattered of the unconformity deposits (recent remobilisation). Voinot et al. (2024) analysed EPE80-319.5 and EPE59-137.4. Coordinates not published.

δ238U in ‰ (per mil) Values of the same system

Standard : NBL CRM 112-A

ValueRangenMineral or matrixSource
0.21 ‰1remobilised uranium ore (basement-hosted)
Single analysis; per-sample uncertainty not published; sample EPE80-319.5 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 37.35 % U, 1.98 µg/g Tl, 55.99 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …
0.3 ‰1uranium ore (basement-hosted)
Single analysis; per-sample uncertainty not published; sample EPE59-137.4 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 66.37 % U, 1062.73 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …
0.57 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE63-076.6, Eagle Point Extension; bracketing-only δ238U at +0.57; 238U/235U of 137.915; about -0.03 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.85 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE80-319.5, Eagle Point Extension; bracketing-only δ238U at +1.05; 238U/235U of 137.953; about +0.25 ‰ after removing the 0.60 ‰ offset specific to this study; same sample as Voinot et al. (2024), published at +0.21 ‰.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.56 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE44-236, Eagle Point Extension; bracketing-only δ238U at +0.43; 238U/235U of 137.914; about -0.04 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.6 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE44-251, Eagle Point Extension; bracketing-only δ238U at +0.51; 238U/235U of 137.919; about 0.00 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.63 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE44-317, Eagle Point Extension; bracketing-only δ238U at +0.75; 238U/235U of 137.923; about +0.03 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.9 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE59-137.4, Eagle Point Extension; bracketing-only δ238U at +0.78; 238U/235U of 137.96; about +0.30 ‰ after removing the 0.60 ‰ offset specific to this study; same sample as Voinot et al. (2024), published at +0.30 ‰.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.54 ± 0.1 ‰1becquerelite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EPE 72-280.6, Eagle Point; bracketing-only δ238U at +0.50; 238U/235U of 137.911; about -0.06 ‰ after removing the 0.60 ‰ offset specific to this study; secondary U(VI) mineral.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.37 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample H-779-57, Eagle Point; bracketing-only δ238U at +0.42; 238U/235U of 137.887; about -0.23 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.78 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EP-2, Eagle Point; bracketing-only δ238U at +0.71; 238U/235U of 137.945; about +0.18 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0.5 ± 0.1 ‰1uraninite
Single analysis; ± 0.10 ‰ (2 SD, reproducibility); sample EP222-215.5, Eagle Point; bracketing-only δ238U at +0.51; 238U/235U of 137.905; about -0.10 ‰ after removing the 0.60 ‰ offset specific to this study.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…

δ234U in ‰ (per mil) Values of the same system

Standard : équilibre séculaire

ValueRangenMineral or matrixSource
158.91 ‰1remobilised uranium ore (basement-hosted)
Single analysis; per-sample uncertainty not published; sample EPE80-319.5 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 37.35 % U, 1.98 µg/g Tl, 55.99 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …
279 ‰1uranium ore (basement-hosted)
Single analysis; per-sample uncertainty not published; sample EPE59-137.4 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 66.37 % U, 1062.73 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …
2 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE63-076.6, Eagle Point Extension.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
−217 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE80-319.5, Eagle Point Extension; 234U deficit: uranium loss within the last 2.5 Myr; Voinot et al. (2024) report +158.91 ‰ on the same sample.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
−19 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE44-236, Eagle Point Extension.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
41 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE44-251, Eagle Point Extension; 234U excess: uranium gain within the last 2.5 Myr.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
19 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE44-317, Eagle Point Extension.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
281 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EPE59-137.4, Eagle Point Extension; 234U excess: uranium gain within the last 2.5 Myr; Voinot et al. (2024) report +279 ‰ on the same sample.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
−1 ‰1becquerelite
Single analysis; per-sample uncertainty not published; sample EPE 72-280.6, Eagle Point; secondary U(VI) mineral.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
0 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample H-779-57, Eagle Point.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
1 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EP-2, Eagle Point.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…
3 ‰1uraninite
Single analysis; per-sample uncertainty not published; sample EP222-215.5, Eagle Point.
Uvarova et al. (2014), Variations in the uranium isotopic compositions of uranium ores fr…

ε205Tl in ε units (parts per 10,000) Values of the same system

Standard : NIST SRM 997

ValueRangenMineral or matrixSource
5 ± 0.6 ε1remobilised uranium ore (basement-hosted)
Single analysis; ± 0.6 (2 SD); sample EPE80-319.5 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 37.35 % U, 1.98 µg/g Tl, 55.99 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …

δ97Mo in ‰ (per mil) Values of the same system

Standard : NIST SRM 3134

ValueRangenMineral or matrixSource
−6.7 ± 0.2 ‰1remobilised uranium ore (basement-hosted)
Single analysis; ± 0.2 (2 SD); sample EPE80-319.5 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 37.35 % U, 1.98 µg/g Tl, 55.99 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …
−2.2 ± 0.2 ‰1uranium ore (basement-hosted)
Single analysis; ± 0.2 (2 SD); sample EPE59-137.4 (assigned to Eagle Point (Athabasca) after Uvarova et al., 2014); IAEA class 7.2 Basement Hosted (Proterozoic unconformity); average age used 1850 Ma; 66.37 % U, 1062.73 µg/g Mo.
Voinot et al. (2024), Tl, Mo and U isotopes in U-ore deposits record Earth's fundamental …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Eagle Point (Athabasca), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/eagle-point-athabasca/ (accessed 2026-10-16).

@misc{isofind2026eaglepointathabascaisotopesig,
  title = {Eagle Point (Athabasca), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/eagle-point-athabasca/},
  note = {Accessed 2026-10-16}
}

Updated : 2026-10-16