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Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province

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Abstract

The contents of radioactive elements and the uranium isotopic composition of kimberlite in the Arkhangelskaya pipe at the M.V. Lomonosov deposit and of nearby country rocks have been studied. A surplus of 234U isotope has been established in rocks from the near-pipe space. The high γ = 234U/238U ratio is controlled by the geological structure of the near-pipe space. A nonequilibrium uranium halo reaches two pipe diameters in size and can be regarded as a local ore guide for kimberlite discovery. The rocks in the nearpipe space are also characterized by elevated or anomalous U, Th, and K contents with respect to the background.

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  1. Institute of Geodynamics and Geology, Laverov Federal Research Center for Comprehensive Study of the Arctic Region, Russian Academy of Sciences, Arkhangelsk, 163000, Russia

    G. P. Kiselev, E. Yu. Yakovlev & S. V. Druzhinin

  2. OAO Severalmaz, Arkhangelsk, 163000, Russia

    A. S. Galkin

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  1. G. P. Kiselev
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  2. E. Yu. Yakovlev
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  3. S. V. Druzhinin
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  4. A. S. Galkin
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Correspondence to E. Yu. Yakovlev.

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Original Russian Text © G.P. Kiselev, E.Yu. Yakovlev, S.V. Druzhinin, A.S. Galkin, 2017, published in Geologiya Rudnykh Mestorozhdenii, 2017, Vol. 59, No. 5, pp. 401–418.

† Deceased.

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Kiselev, G.P., Yakovlev, E.Y., Druzhinin, S.V. et al. Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province. Geol. Ore Deposits 59, 391–406 (2017). https://doi.org/10.1134/S1075701517050014

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