Material composition of calcite carbonatites of the kovdor massif that are potential industrial ores

Authors

  • Ксения Дмитриевна Степанова Saint-Petersburg Mining University
  • Сергей Викторович Петров St Petersburg University image/svg+xml

DOI:

https://doi.org/10.17308/geology.2018.1/1442

Keywords:

Kovdor massif, apatite-carbonate ores, calcite carbonatites, apatite, technological grades of ore

Abstract

The Kovdor massif of alkaline, ultrabasic and carbonatite rocks is one of the brightest representatives in the family of similar complexes in Karelian-Kola region. This research presents the results of study material composition of ores that are located in the apatite-carbonate deposit at the SouthEastern part of the Kovdor massif. These ores are divided into basic technological classes according to the content of P2O5 in vol. %: poor (< 1,5), common (1,5–3) and rich (> 3). Mineralogical and petro-graphic studies were carried out using the optical, x-ray and electron microscopic methods. We have estimated relative abundances which allowed allocating main, minor and accessory minerals. The chemical composition of minerals has been determined. The crystalline forms of minerals, size of its and their textural and structural features have been described in this study. Accordingly, we have educed that above-named mineral characteristics are representative for deposit of this type.

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Author Biographies

  • Ксения Дмитриевна Степанова, Saint-Petersburg Mining University

    postgraduate student of the Department of Geology and Mineral Deposits Prospecting

  • Сергей Викторович Петров, St Petersburg University

    Associate Professor of the Department of Geology of Mineral Deposits, Candidate of Geological and Mineralogical Sciences

References

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Published

2018-02-12

Issue

Section

Geology, Prospecting and Exploration of Solid Minerals, Minerageny

How to Cite

Material composition of calcite carbonatites of the kovdor massif that are potential industrial ores. (2018). Proceedings of Voronezh State University. Series: Geology, 1, 102-108. https://doi.org/10.17308/geology.2018.1/1442