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Eucrite
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Eucrites are stony , many of which originate from the surface of the 4 Vesta and are part of the clan. They are the most common achondrite group with over 100 meteorites found.

Eucrites consist of rock from the crust of 4 Vesta or a similar parent body. They are mostly composed of -poor , , and calcium-rich ().B. Mason: Meteorites. John Wiley, New York 1962.

Based on differences of chemical composition and features of the component crystals, they are subdivided into several groups:Mittlefehldt, McCoy, Goodrich and Kracher: Non-chondritic Meteorites from Asteroidal Bodies, In: Reviews in Mineralogy Vol. 36, Planetary Materials, Mineralogical Society of America, 1998.

  • Non-cumulate eucrites are the most common variety and can be subdivided further:
    • Main series eucrites formed near the surface and are mostly under the pressure of overlying newer deposits.
    • Stannern trend eucrites are a rare variety.
    • Nuevo Laredo trend eucrites are thought to come from deeper layers of 4 Vesta's crust, and are a transition group towards the cumulate eucrites.
  • Cumulate eucrites are rare types with oriented crystals, thought to have solidified in magma chambers deep within 4 Vesta's crust.
  • Polymict eucrites are consisting of mostly eucrite fragments and less than one part in ten of . They are less common.


Etymology
Eucrites get their name from the Greek word eukritos meaning "easily distinguished". This refers to the silicate minerals in them, which can be easily distinguished because of their relatively large grain size.

Eucrite is also a now obsolete term for -, an formed in the Earth's crust. The term was used as a rock type name for some of the igneous rocks of Scotland.Sutherland, D. S. (1982) Igneous Rocks of the British Isles, Chichester, John Wiley, page 536.


See also
  • Glossary of meteoritics


External links

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