RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES3002, doi:10.2205/2006ES000196, 2006

2006ES000196-fig09.html
Figure 9. Typical Cr ores of the Polar Urals. Polished platelets, scaled 1/2. (a) Nodular rich disseminated chromite ore. Rai-Iz Massif, Enganskoe-II ore occurrence. (b) Medium-grade disseminated chromite ore. Rai-Iz Massif, Tsentralnoe deposit. (c) Brecciated rich disseminated Cr ore with dunite and uvarovite veinlets in DVC dunite. Voikar-Syninskii Massif. (d) Stockwork lean metamorphosed Cr ore with kemmererite. Syum-Keu Massif, Nyaro-Pe block.

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Citation: Makeyev, A. B. (2006), Typomorphic features of Cr-spinel and mineralogical prospecting guides for Cr ore mineralization, Russ. J. Earth Sci., 8, ES3002, doi:10.2205/2006ES000196.

Copyright 2006 by the Russian Journal of Earth Sciences
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