Chrome spinels and accessory mineralization in the weathering crust of the Vladimir deposit, Varshavsky ultramafic massif, southern Urals

The paper presents the characteristics of chrome spinels from an ore-bearing packet of the Vladimir chromite deposit. Three main types of chrome spinels are distinguished by morphology and chemical composition: medium-chrome ore-forming, high-chrome transformed, and low-chrome relict accessory. The...

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Veröffentlicht in:Geology of ore deposits 2016-12, Vol.58 (8), p.697-710
Hauptverfasser: Ankushev, M. N., Zaykov, V. V., Kotlyarov, V. A., Romanenko, M. E.
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container_end_page 710
container_issue 8
container_start_page 697
container_title Geology of ore deposits
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creator Ankushev, M. N.
Zaykov, V. V.
Kotlyarov, V. A.
Romanenko, M. E.
description The paper presents the characteristics of chrome spinels from an ore-bearing packet of the Vladimir chromite deposit. Three main types of chrome spinels are distinguished by morphology and chemical composition: medium-chrome ore-forming, high-chrome transformed, and low-chrome relict accessory. The significant role of weathering conditions is expressed in alteration of accessory chrome spinel. The formation of high-chrome spinels is explained by the hydrothermal effect of the Varshavsky granitoid massif with accompanying dikes and talc–carbonate metasomatic rocks. Characteristic accessory minerals are represented by native gold and nickel, millerite, pentlandite, chalcopyrite, maucherite, PGE sulfides, and picroilmenite.
doi_str_mv 10.1134/S1075701516080031
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subjects Carbonates
Chalcopyrite
Chemical composition
Chromite
Dikes
Earth and Environmental Science
Earth Sciences
Embankments
Gold
Mineral Resources
Mineralization
Minerals and Mineral Assemblages
Morphology
Nickel
Nickel ores
Organic chemistry
Pentlandite
Spinel
Talc
Weathering
title Chrome spinels and accessory mineralization in the weathering crust of the Vladimir deposit, Varshavsky ultramafic massif, southern Urals
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