Abstract
Mineral-petrographic studies of interaction between sulfide iron minerals and magnetite and its effect on processing characteristics of ferruginous quartzite, Kursk Magnetic Anomaly (KMA), are reported. The ferruginous quartzite classification was developed by the sulfide factor in terms of specific textural and structural features of mineral components to be separated.
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References
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V. A. Chanturia, Perspectives of Sustainable Development of Mining and Mineral Processing Industries in Russia [in Russian], Ruda Metally, Moscow (2008).
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Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaeykh, No. 5, pp. 95–98, September–October, 2009
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Chanturia, E.L., Gzogyan, S.P. Features of sulfide ferruginous quartzite mineralization. J Min Sci 45, 495–498 (2009). https://doi.org/10.1007/s10913-009-0061-2
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DOI: https://doi.org/10.1007/s10913-009-0061-2