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Hexahedrite

In this article, we will delve into the fascinating world of Hexahedrite. We will explore its origins, its evolution over time and its impact on different aspects of daily life. Hexahedrite has been the subject of study and debate for many years, and its relevance is still evident in today's world. Through this article, we aim to shed light on Hexahedrite, analyzing its importance and influence in today's society. Join us on this journey to discover more about Hexahedrite and its role in the contemporary world.

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Hexahedrite
— Structural class —
Neumann bands in the Sikhote-Alin meteorite
Compositional typeIron
CompositionKamacite
A phase diagram showing the link between structural and chemical classification. Hexahedrites contain mostly kamacite because their chemistry only allows kamacite as a stable phase.

Hexahedrites are a structural class of iron meteorite. They are composed almost exclusively of the nickeliron alloy kamacite and are lower in nickel content than the octahedrites.[1] The nickel concentration in hexahedrites is always below 5.8% and only rarely below 5.3%.[2]

The name comes from the cubic (i.e. hexahedron) structure of the kamacite crystal. After etching, hexahedrites do not display a Widmanstätten pattern, but they often do show Neumann lines: parallel lines that cross each other at various angles, and are indicative of impact shock on the parent body. These lines are named after politician Johann Georg Neumann who discovered them in 1848.[3]

Chemical classification

Concentrations of trace elements (germanium, gallium and iridium) are used to separate the iron meteorites into chemical classes, which correspond to separate asteroid parent bodies. Chemical classes that include hexahedrites are:[4]

See also

References

  1. ^ Buchwald, Vagn F. (1975). Handbook of Iron Meteorites. Vol. 1–3. University of California Press. OCLC 928839971.
  2. ^ Wasson, J.T. (1985). Meteorites: Their Record of Early Solar-System History. W. H. Freeman. ISBN 9780716717003.
  3. ^ Burke, J.G. (1991) . "Note 63. Schreibers (1820), 70–72". Cosmic Debris: Meteorites in History. University of California Press. p. 339. ISBN 9780520073968.
  4. ^ Wasson, J.T. (2012) . "C. Classification of Metal-Rich Meteorites". Meteorites: Classification and Properties. Springer. pp. 47–. ISBN 9783642658631.