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Genetic Nature of Mineralization with Native and Intermetallic Compounds in the Bobruisk Ring Structure (Republic of Belarus)

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Abstract

The results of study of the Bobruisk ring structure (Republic of Belarus) containing ~80 rare rockforming and accessory minerals are reported. Among them are native (Fe, Cu, Sn, Zn, Pb, Ag, Mo, W, Al) and intermetallic (Fe, Cr, Ni, Mo, B, N, C, Si) compounds, natural alloys (Fe–Cr, Fe–Cr–Mo–W–B; brass (Cu–Zn–Pb); and bronze (Sn–Pb–Zn–Cu)). They are observed as segregations of various shapes and sizes, as well as their aggregates. The formation of mineralization is controlled by reduced mantle fluids enriched in H2, CH4, CO, Si, N, and O and stimulating accumulation of rare elements as native and intermetallic phases, alloys, rather than isomorphic impurities in minerals.

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Authors and Affiliations

  1. Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences, Irkutsk, 650033, Russia

    V. I. Levitskiy, L. A. Pavlova & I. V. Levitskiy

  2. Research and Productive Center for Geology, Minsk, 220141, Republic of Belarus

    V. V. Solodilova & N. S. Zavadich

Authors
  1. V. I. Levitskiy
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  2. V. V. Solodilova
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  3. N. S. Zavadich
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  4. L. A. Pavlova
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  5. I. V. Levitskiy
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Correspondence to V. I. Levitskiy.

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Original Russian Text © V.I. Levitskiy, V.V. Solodilova, N.S. Zavadich, L.A. Pavlova, I.V. Levitskiy, 2018, published in Doklady Akademii Nauk, 2018, Vol. 481, No. 2.

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Levitskiy, V.I., Solodilova, V.V., Zavadich, N.S. et al. Genetic Nature of Mineralization with Native and Intermetallic Compounds in the Bobruisk Ring Structure (Republic of Belarus). Dokl. Earth Sc. 481, 857–861 (2018). https://doi.org/10.1134/S1028334X18070140

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  • DOI: https://doi.org/10.1134/S1028334X18070140

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