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

2006ES000196-fig03.html
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.

RJES

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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