D'Orbigny
The D'Orbigny meteorite was found during July 1979 while ploughing a rock-less field in
the south of the Buenos Aires Province, Argentina. Because of
its shape it was believed to be an Indian artefact, in
particular a mortar, and was kept at the farm. It was later
suspected of being a meteorite in 1998 and in 2000 a sample was
identified in Vienna as being a very rare Angrite.
The stone had a mass of 16.55
kg and had a peculiar shape, somewhat like a loaf of bread but
with a gently sloped and fusion crust-covered front with
regmaglypts and a concave back side. The front and back sides
consist of a medium to coarse-grained ophitic textured rock with
a heterogeneous, highly porous coarse-grained rock sandwiched
between them. The major minerals are augite, anorthite and
olivine. Augite is very common in irregularly shaped open
druses. There it forms euhedral elongated prismatic crystals and
has a chemical composition similar to the cores of rock-forming
augites. Anorthite forms laths which commonly include some
olivine or augite. The dense portions of D’Orbigny resembles Asuka
881371 and Sahara 99555 while with the latter, D’Orbigny shares
the presence of abundant round vugs. Olivine is very common in
the shells of the abundant vugs/hollow spheres. Large (up to
centimetre-sized) olivines are scattered throughout D’Orbigny
mimicking xenocrysts or forming Olivinite. D’Orbigny is unique
in its overall structure, its richness in hollow spheres, the
presence of abundant druses containing perfectly crystallized
augites and anorthites, the presence of abundant glass and the
presence of olivinite rocks with olivines of highly magnesian
composition, comparable to olivine xenocrysts from Asuka 881371.
This partslice
is most likely from the central porous region of the D'Orbigny
stone. Vugs/vesicles can clearly be seen alongside the highly
porous course-grained matrix. While a little difficult to see in
the photos, the vugs do have an extremely thin layer of olivine
while a larger crystal is evident to the left. Much of this
piece is also occupied by the abundant and irregularly shaped
open druses mentioned above. This specimen of the highly unique
D'Orbigny meteorite is part of the Meteorites Australia Collection
(MA.05.0088).
D’Orbigny: A new and unusual Angrite.
G. Kurat, F. Brandstätter, R. Clayton, M. A. Nazarov, H. Palme, L. Schultz, M. E. Varela, E. Wäsch, H. W. Weber and G. Weckwerth. (500kb)
D’Orbigny: A new window into Angrite genesis.
G. Kurat, M. E. Varela, F. Brandstätter, E. Wäsch and M. A.
Nazarov.
(165kb)
Petrology and geochemistry of D’Orbigny, geochemistry of Sahara 99555, and the origin of Angrites.
David W. Mittlefehldt, Marvin Killgore and Michael T. Lee. (3.49MB)
D'Orbigny (Angrite) - 1.25g Partslice
D'Orbigny (Angrite) - 1.25g Partslice
D'Orbigny (Angrite) - 1.25g Partslice (Annotated close-up of interior)
D'Orbigny (Angrite) - 1.25g Partslice (Close-up of interior)
D'Orbigny (Angrite) - 1.25g Partslice (Close-up of vesicle)
D'Orbigny (Original Uncut Mass) -
Source:
D’Orbigny: A new window into Angrite genesis.
Click here to view the archive of the Monthly Favourites
|