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Palabora

Limpopo, Phalaborwa carbonatite complex, South Africa

Magmatic (Ni-Cu-PGE, carbonatites)Cu-P (U)

Type
Intrusive uranium

Deposit of the high-temperature redox category in the study of uranium ore concentrates (yellowcake) from 40 mines. Uranium reduced at high temperature (igneous or metamorphic processes): clustered 238U/235U, indistinguishable from the non-redox conglomerates (common mean 137.833 ± 0.034, 2SD), and 235U/234U close to secular equilibrium (Brennecka et al., 2010). By-product uranium of the copper-bearing carbonatite complex; high ratio for its category. Foskor and Phalaborwa apatite with Sr much more radiogenic (0.7114) than Kola apatite (0.7033) and δ238U close to 0 (Hill et al., 2024). Indicative coordinates (Phalaborwa).

238U/235U isotope ratio, no unit Values of the same system

Standard : CRM 129-A (rapport absolu, double traceur 236U-233U)

ValueRangenMineral or matrixSource
137.865 ± 0.0181uranium ore concentrate (yellowcake)
Single analysis; high-temperature redox category; by-product uranium of the copper-bearing carbonatite complex; high ratio for its category.
Brennecka et al. (2010), Natural variations in uranium isotope ratios of uranium ore conc…

235U/234U isotope ratio, no unit Values of the same system

Standard : CRM 129-A (rapport absolu, double traceur 236U-233U)

ValueRangenMineral or matrixSource
132.02 ± 0.421uranium ore concentrate (yellowcake)
Single analysis; high-temperature redox category.
Brennecka et al. (2010), Natural variations in uranium isotope ratios of uranium ore conc…

87Sr/86Sr isotope ratio, no unit Values of the same system

Standard : NIST SRM 987

ValueRangenMineral or matrixSource
0.711435 ± 0.0000130.711426 / 0.7114452magmatic phosphate (bulk)
Mean and standard deviation recalculated from 2 analyses, samples ZA-A, ZA-B; ZA-A from Foskor, ZA-B from Phalaborwa (carbonatite complex apatite, Hill et al., 2024).
Hill et al. (2024), Reconstructing the depositional environment and diagenetic modificati…

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

Standard : NBL CRM 112-A

ValueRangenMineral or matrixSource
0.029 ± 0.066 ‰1magmatic apatite (leached fraction)
Single analysis; sample ZA-A; ZA-A from Foskor, ZA-B from Phalaborwa (carbonatite complex apatite, Hill et al., 2024).
Hill et al. (2024), Reconstructing the depositional environment and diagenetic modificati…

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

Standard : équilibre séculaire

ValueRangenMineral or matrixSource
0.33 ± 13.85 ‰1magmatic apatite (leached fraction)
Single analysis; sample ZA-A; a departure from 0 signals uranium mobility within the last two million years; ZA-A from Foskor, ZA-B from Phalaborwa (carbonatite complex apatite, Hill et al., 2024).
Hill et al. (2024), Reconstructing the depositional environment and diagenetic modificati…

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
8.63 ‰1magmatic apatite (PO4 oxygen)
Single analysis; sample ZA-B; ZA-A from Foskor, ZA-B from Phalaborwa (carbonatite complex apatite, Hill et al., 2024).
Hill et al. (2024), Reconstructing the depositional environment and diagenetic modificati…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Palabora, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/palabora/ (accessed 2026-10-15).

@misc{isofind2026palaboraisotopesignatures,
  title = {Palabora, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/palabora/},
  note = {Accessed 2026-10-15}
}

Updated : 2026-10-15