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

2006ES000196-fig10.html
Figure 10. Microprobe scanning profiles (Camebax Microbeam microprobe, characteristic radiation) across a zonal Cr-spinel grain. The reversed zoning was caused by the metamorphic transformation of Cr-picotite into Cr-magnetite along a crack intersecting the grain core.

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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