RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES4001, doi:10.2205/2005ES000181, 2005

Figure 9. Zonal chromite grain in lherzolite I1063/17. The brighter
central part of the grain corresponds to Fe-richer chromite
(Table 6, analysis I1063/17-7(c)), and its grayish peripheral part corresponds
to Mg-richer chromite (Table 6, analysis I1063/17-8(r)); dark gray
grains are olivine. The sample is cut by serpentine veinlets with
small magnetite grains (white) and a younger serpentine-chlorite
veinlet. BSE image, CamScan electron microscope, Moscow State
University.

Citation: Sharkov, E. V., N. S. Bortnikov, T. F. Zinger, and A. V. Chistyakov (2005), Silicic Fe-Ti-oxide series of slow-spreading ridges: petrology, geochemistry, and genesis with reference to the Sierra Leone segment of the Mid-Atlantic Ridge axial zone at 6° N, Russ. J. Earth Sci., 7, ES4001, doi:10.2205/2005ES000181.
Copyright 2005 by the Russian Journal of Earth Sciences
Powered by TeXWeb (Win32, v.2.0).