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Streltsovskoye

Eastern Transbaikalia, Streltsovsk ore field (Krasnokamensk), Russia

UraniumU (Mo)

Type
Hydrothermal uranium veins (pitchblende)

Streltsovsk ore field, linked to a Mesozoic caldera (felsic volcanics and granites), Russia's leading uranium district; spherulitic pitchblende at about 135 ± 3 Ma. Namesake deposit of the field. 238U/235U ratio measured by Chernyshev et al. (2014): uranium of the early growth zones of pitchblende crusts heavier (by 0.22 to 0.45 ‰) than that of the latest zones, nuclear volume fractionation during reduction of U(VI) to U(IV). Indicative coordinates (Streltsovsk field).

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

Standard : NBL CRM 112-A

ValueRangenMineral or matrixSource
137.7945 ± 0.00495137.791 / 137.7982spherulitic pitchblende crust (85/67)
Mean and standard deviation recalculated from 2 analyses, first and last growth zones; equivalent δ238U -0.33 to -0.28 ‰.
Chernyshev et al. (2014), 238U/235U isotope ratio variations in minerals from hydrotherma…

Deposits of the same type

Cite this page

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

@misc{isofind2026streltsovskoyeisotopesignatur,
  title = {Streltsovskoye, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/streltsovskoye/},
  note = {Accessed 2026-10-15}
}

Updated : 2026-10-15