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

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.

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
Powered by TeXWeb (Win32, v.2.0).