Hi Melanie, Jeff, Werner, and List,

BARRAT J.A. et al. (1999) The Tatahouine diogenite: Mineralogical
and chemical effects of sixty-three years of terrestrial residence
(MAPS 34-1, 1999, 091-097, excerpts):

"The crystals of orthopyroxene ... contain many inclusions ... of silica, 
troilite,
 chromite, and *metal*. The silica inclusions ... contain silica with either 
metal
 (Fe, 98%; Ni + Co, 2%) or chromite."

and:

"The samples collected in 1994 contain secondary minerals, which clearly 
developed
in the soil during their 63 years of terrestrial residence. First, *Fe stains* 
replace metal
or troilite inclusions on the surfaces of the clasts in contact with soil or 
inside fractures.
Second, yellowish to *light orange calcitic aggregates* were found in some 
samples.
They mainly occur as a partial filling with a rosette texture or completely 
fill some
fractures (ca. 100 µm wide)."

Best wishes,

Bernd

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