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Andradite
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Andradite is a species of the . It is a nesosilicate, with formula Ca3Fe2Si3O12.

Andradite includes three varieties:

  • : a historical variety found in the Scandinavian islands, brownish or reddish in color, often opaque or translucent. Olga Bortnik. All about precious stones. ― Moscow: Harvest, 2011.
  • : Vivid green in color, one of the most valuable and rare stones in the world.
    (2025). 9780226305110, University of Chicago Press. .
  • Melanite: Black in color due to limited substitution of for iron. Also known as "titanian andradite". Forms a solid solution with and depending on titanium and iron content. Melanite, Mindat.org
  • Topazolite: Yellow-green in color and sometimes of high enough quality to be cut into a faceted , it is rarer than demantoid.

It was first described in 1868 for an occurrence in , , . Andradite was named after the statesman, naturalist, professor and poet José Bonifácio de Andrada e Silva (1763–1838).


Occurrence
It occurs in developed in contact metamorphosed impure or calcic ; in chlorite and and in alkalic (typically ). Associated minerals include , , , , , dolomite and . It is found in , , the of , and and in Dnipropetrovsk Oblast in .

Like the other garnets, andradite crystallizes in the cubic 3}}d, with unit-cell parameter of 12.051 Å at 100 K.Thomas Armbruster and Charles A. Geiger (1993): " Andradite crystal chemistry, dynamic X-site disorder and structural strain in silicate garnets." European Journal of Mineralogy v. 5, no. 1, p. 59-71.

The of andradite contains two mutually canted equivalent antiferromagnetic sublatticesDanylo Zherebetskyy (2010). Quantum mechanical first principles calculations of the electronic and magnetic structure of Fe-bearing rock-forming silicates, PhD Thesis, Universal Publishers/Dissertation.com, Boca Raton, Florida, USA, p. 136. . below the Néel temperature (TN=11 KEnver Murad (1984): " Magnetic ordering in andradite." American Mineralogist 69, no. 7-8; pp. 722–24.).


See also


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