Hello Tracy, Zélimir, Marcin, and List,

PRZYLIBISKI T.A. et al. (2005) The Zaklodzie enstatite
meteorite: Mineralogy, petrology, origin and classification
(MAPS 40-9, 2005, pp. A185-A200, excerpt from p. A191):

"No qualitative differences in mineral composition were found between the three 
zones
of the meteorite. The observed color differences result from higher 
concentrations of
very fine, disseminated graphite inclusions in the two outer zones and the 
locally rusty
color is due to weathering. In the lighter internal zone, graphite forms fairly 
large
aggregates."


Best regards,

Bernd

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