 | Vigdergauz, V. E., Makarov, D. V., Zorenko, I. V., Belogub, E. V., Malyarenok, M. N., Shrader, E. A., Kuznetsova, I. N. (2008) Effect exerted by structural features of copper-zinc ores on their oxidation and technological properties. Journal of Mining Science, 44 (4) 413-420 doi:10.1007/s10913-008-0046-6 | Journal (article/letter/editorial) | | mineral phases, namely, gannigite, biankite, chalcanthite, which relate with sulfate generating on evaporation...Copper-zinc ores concentrate mainly in the Urals in Russia. Massive copper-zinc-pyritic ores are the most...Academy of Sciences, E-mail: vigderg@mail.ru, Moscow, Russia. *Institute of Chemistry and Technology of Rare...E-mail: makarovdv@chemy.kolasc.net.ru, Apatity, Russia. **Institute of Mineralogy, Ural Branch, Russian...of Sciences, E-mail: bel@mineralogy.ru, Miass, Russia. Translated from Fiziko-Tekhnicheskie Problemy |  | | Journal (article/letter/editorial) | | Miass, Russia Geological Department, Saint-Petersburg State University, Saint-Petersburg, Russia c Natural...Cyprus, Uralian and Kuroko type in the South Urals, Russia, have been studied. Specific subzones enriched...considered analogous to Cyprus-type deposits (e.g., Letnee); (3) Zn-rich massive sulphide Cu-deposits of Urals...economical significance in only some deposits (e.g., Letnee). They are the alteration products of chalcopyrite...to several tenths of wt.%. Some covellite from Letnee is enriched in Se up to about 2 wt.% (estimated |  | | Conference Proceedings (Volume) | | basement of west Magnitogorsk Arc, the Southern Urals, Russia .................................................Volcanic-hosted massive sulfide deposits of the Urals, Russia: evidence for a magmatic contribution of metals...polymetallic skarn ores at Pitkäranta, Ladoga Karelia, Russia ....................... 1555 .................polycyclic orogeny: the example of the Litsa district, Russia Anne-Sylvie André-Mayer, Michel Cuney, Julien...ic and alkaline gabbroic complexes in Karelia, Russia .. ........................................... |
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