We are very pleased to offer this spectacular Eucrite-NWA 3368 (which can be found on p. 120 of "The Field Guide to Meteors and Meteorites" by L. Chitwood and the late O. Richard Norton!) This is a visually striking Eucrite, having large diogenite clasts and extremely fine grained basaltic clasts set in a light matrix having a pink hue! Many of the larger slices have sizeable pieces of metal showing also! NWA 3368 is a single stone weighing 1623 grams before cutting losses. After cutting losses and type specimens donated for scientific research, only around 1300 grams remains for collectors. This is a very beautiful eucrite, and the scientists that classified it dubbed it the "pink eucrite". All slices cut perfectly and very thin (~2mm) to give the optimal display area to weight ratio, and are expertly finished on both sides. Each specimen comes in a Museum Grade membrane display case.
Classification Data
Official Classification Name: NWA 3368
Classification: Polymict Eucrite
The following was submitted to Mike Zolensky by Dolores Hill on in
early
September:
"Microprobe analyses conducted on a small matrix chip confirm that the
sample
is a eucrite (pyroxene Wo6En36Fs59 and Wo40En30Fs30; plagioclase
An90Ab10Or0.4). Chromite containing 5-27% TiO2 and ~5% Al2O3 &
ilmenite are
present. In hand specimen, the sample appears to be a polymict
eucrite.
There are a variety of clasts ranging in size from several mm to ~ 2
cm.
Diogenite clasts, dark, angular clasts, and rounded grains, are set in
a light
matrix typical of eucrites except for its distinct pink hue. There is
some "foliation" in this coloration: approximately half of the slice is
slightly darker pink than the other; with an indistinct, irregular
boundary."
General Observations: (By Kathryn Gardner while on the e-probe)
Major Mineralogy: High Ca Pyroxene, Low Ca Pyroxene, Plagioclase
Minor Mineralogy: High and Low Titanium Chromite, Troilite, Ilmenite,
Silica,
Fe metal, Phosphates
Mg #�s for clinopyroxenes: ~52-53 (average)
Mg #�s for orthopyroxenes: ~37-38 (average)
Total Fe/Mn: ~30 (standard for eucrites)
Oxygen isotope data fit in with other eucrites.
Oxide grains often exsolved to a varied extent.
Both pyroxenes seem so far to have the same composition, although both
fine-
grained and coarse-grained components exist.
The specimens currently available are below:
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