That unweathered inner part of Zaklodzie had very distinct edges; I was also
surprised to see the (relatively) huge metal blebs in the slices. I would
think that there would be an area of most weathering closest to the
exterior, and a more graduated progression as the elements slowly seeped
into the interior, rather than a discrete 'core', which looked very
eucrite-ish. Is there any chance that this was an anomalous piece of
Zaklodzie with an inclusion? What created such a clear boundary?
Tracy Latimer
Hi
I think that the most competent answer You will find here.
Przylibski T. A. et al.
The Zaklodzie enstatite meteorite: Mineralogy, petrology, origin and
classification,
/Meteoritics and Planetary Science /40, Nr 9, A185-A200 (2005).
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