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Andradite





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(Redirected from Melanite)
 


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

Andradite [Adr]

Single crystal (4.2 cm) – Diakon, Nioro du Sahel Circle, Kayes Region, Mali

General

Category

Garnet group

Formula
(repeating unit)

Ca3Fe2(SiO4)3

IMA symbol

Adr[1]

Strunz classification

9.AD.25

Crystal system

Cubic

Crystal class

Hexoctahedral (m3m)
H-M symbol: (4/m 3 2/m)

Space group

Ia3d

Unit cell

a = 12.056 Å; Z = 8

Identification

Color

Yellow, greenish yellow to emerald-green, dark green; brown, brownish red, brownish yellow; grayish black, black; may be sectored

Crystal habit

Commonly well-crystallized dodecahedra, trapezohedra, or combinations, also granular to massive

Cleavage

none

Fracture

conchoidal to uneven

Tenacity

Brittle

Mohs scale hardness

6.5 to 7

Luster

Adamantine to resinous, dull

Streak

White

Diaphaneity

Transparent to translucent

Specific gravity

3.859 calculated; 3.8–3.9 measured

Optical properties

Isotropic, typically weakly anisotropic

Refractive index

n = 1.887

Absorption spectra

demantoid – 440 nm band or complete absorption at 440 nm and below, may also have lines at 618, 634, 685, 690 nm[2]

References

[2][3][4][5]

Major varieties

Demantoid

transparent light to dark green to yellow-green

Melanite

opaque black

Topazolite

transparent to translucent yellow, may show chatoyancy

Andradite includes three varieties:

It was first described in 1868 for an occurrence in Drammen, Buskerud, Norway.[3][4][7] Andradite was named after the Brazilian statesman, naturalist, professor and poet José Bonifácio de Andrada e Silva (1763–1838).[3][7]

Occurrence

edit

It occurs in skarns developed in contact metamorphosed impure limestones or calcic igneous rocks; in chlorite schists and serpentinites and in alkalic igneous rocks (typically titaniferous). Associated minerals include vesuvianite, chlorite, epidote, spinel, calcite, dolomite and magnetite.[3] It is found in Iran, Italy, the Ural MountainsofRussia, Arizona and California and in Dnipropetrovsk OblastinUkraine.

Like the other garnets, andradite crystallizes in the cubic space group [[Ia3d]], with unit-cell parameter of 12.051 Å at 100 K.[9]

The spin structure of andradite contains two mutually canted equivalent antiferromagnetic sublattices[10] below the Néel temperature (TN=11 K[11]).

See also

edit
  • Geology
  • Grossular
  • Mineral
  • Mineral collecting
  • Pyrope
  • Spessartine
  • Tsavorite
  • Uvarovite
  • References

    edit
    1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  • ^ a b Gemological Institute of America, GIA Gem Reference Guide 1995, ISBN 0-87311-019-6
  • ^ a b c d Handbook of Mineralogy
  • ^ a b Andradite, Mindat.org
  • ^ Webmineral data
  • ^ Olga Bortnik. All about precious stones. ― Moscow: Harvest, 2011.
  • ^ a b c d Grande, Lance; Augustyn, Allison (2009). Gems and Gemstones: Timeless Natural Beauty of the Mineral World. University of Chicago Press. pp. 188–91. ISBN 978-0-226-30511-0.
  • ^ Melanite, Mindat.org
  • ^ 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.
  • ^ Danylo 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. ISBN 1-59942-316-2.
  • ^ Enver Murad (1984): "Magnetic ordering in andradite." American Mineralogist 69, no. 7-8; pp. 722–24.
  • edit

      Media related to Andradite at Wikimedia Commons


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Andradite&oldid=1222194696"
     



    Last edited on 4 May 2024, at 14:09  





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    This page was last edited on 4 May 2024, at 14:09 (UTC).

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