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

Figure 3. Southern part of the Rai-Iz Massif (as seen from the
Engaiskoe-I occurrence of ore mineralization). Violet rock blocks in
the foreground are Cr ore. The resources of Cr ore at the Engaiskoe
occurrence are 100,000 tons. The serpentine road seen in the middle
distance is used to transport ore from the Tsentraloe deposit. In the
background, Mount Chernaya is seen, with a contact of ultrabasites
(dvc) and gabbroids.

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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