Fine-grained
and powdery, average clast and mineral grain size is
< 2mm with few
clasts > 3 mm. Clast modes: diogenites, 74 vol.
%; eucrites 20
vol. % (12 % cumulate, 8 % basaltic); anorthositic-
like clasts, 3 %;
shock melt clasts. 2 %, and opaques, 1%.
Diogenite
orthopyroxene, Fs35.6-38.8Wo2.3-4.2; plagioclase, An 87;
chromite, Cr/(Cr+Al)
= 0.81; metal, Ni = 0.67 wt %. Melt inclusions
in opx contain
Ca-rich pyroxene, Fs33.3Wo37.5; phosphate,
silica phase, and
K-rich glass. Plagioclase-pyroxene cumulates,
Fs38.2Wo21;
plagioclase, An86.
eucrite textures
include recrystallized,
granular, ophitic,
subophitic, and variolitic
(Fs31.6Wo7 and
Fs61.8Wo33). Plagioclase-rich clasts have 95 vol.%
plagioclase
(An96.1). Mildly shocked; no apparent oxidation or Fe
staining.
Specimens: 26 g,