Template:Short description Template:Use American English Template:Use mdy dates Template:Infobox meteorite subdivision Octahedrites are the most common structural class of iron meteorites. The structures occur because the meteoric iron has a certain nickel concentration that leads to the exsolution of kamacite out of taenite while cooling.

StructureEdit

Template:See also Octahedrites derive their name from the crystal structure paralleling an octahedron. Opposite faces are parallel so, although an octahedron has 8 faces, there are only 4 sets of kamacite plates.

Due to a long cooling time in the interior of the parent asteroids, these alloys have crystallized into intermixed millimeter-sized bands (from about 0.2 mm to 5 cm).<ref name=CdE2009>Template:Cite journal</ref> When polished and acid etched the classic Widmanstätten patterns of intersecting lines of lamellar kamacite, are visible.

In gaps between the kamacite and taenite lamellae, a fine-grained mixture called plessite is often found. An iron nickel phosphide, schreibersite, is present in most nickel-iron meteorites, as well as an iron-nickel-cobalt carbide, cohenite. Graphite and troilite occur in rounded nodules up to several cm in size.<ref name=him1975>Vagn F. Buchwald: Handbook of Iron Meteorites. University of California Press, 1975.</ref>

SubgroupsEdit

File:ZacatecasMeteoriteGDL cropped.JPG
The Zacatecas Meteorite found in 1782 in Zacatecas Mexico, weighing 780kg.

Template:See also Octahedrites can be grouped by the dimensions of kamacite lamellae in the Widmanstätten pattern, which are related to the nickel content:<ref>James H. Shirley,Rhodes Whitmore Fairbridge, Encyclopedia of planetary sciences, Springer, 1997. Template:ISBN</ref>

  • Coarsest octahedrites, lamellae width >3.3 mm, 5–9% Ni, symbol Ogg
  • Coarse octahedrites, lamellae 1.3–3.3 mm, 6.5–8.5% Ni, symbol Og
  • Medium octahedrites, lamellae 0.5–1.3 mm, 7–13% Ni, symbol Om
  • Fine octahedrites, lamellae 0.2–0.5 mm, 7.5–13% Ni, symbol Of
  • Finest octahedrites, lamellae <0.2 mm, 17–18% Ni, symbol Off
  • Plessitic octahedrites, kamacite spindles, a transitional structure between octahedrites and ataxites,<ref>Geochimica et Cosmochimica Acta, Volume 45, Ed. 9–12</ref> 9–18% Ni, symbol Opl

MineralEdit

Octahedrite is an obsolete synonym for anatase, one of the three known titanium dioxide minerals.Template:Cn

See alsoEdit

ReferencesEdit

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External linksEdit

Template:Meteorites