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A n d r a d i t e
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A r t i c l e
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T a l k
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L a n g u a g e
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( R e d i r e c t e d f r o m M e l a n i t e )
Single crystal (4.2 cm ) – Diakon, Nioro du Sahel Circle, Kayes Region, Mali
Garnet group
Ca 3 Fe 2 (SiO4 )3
Adr[1 ]
9.AD.25
Cubic
Hexoctahedral (m 3 m ) H-M symbol : (4/m 3 2/m)
I a 3 d
a = 12.056 Å; Z = 8
Yellow, greenish yellow to emerald-green, dark green; brown, brownish red, brownish yellow; grayish black, black; may be sectored
Commonly well-crystallized dodecahedra, trapezohedra, or combinations, also granular to massive
none
conchoidal to uneven
Brittle
6.5 to 7
Adamantine to resinous, dull
White
Transparent to translucent
3.859 calculated; 3.8–3.9 measured
Isotropic, typically weakly anisotropic
n = 1.887
demantoid – 440 nm band or complete absorption at 440 nm and below, may also have lines at 618, 634, 685, 690 nm [2 ]
[2 ] [3 ] [4 ] [5 ]
transparent light to dark green to yellow-green
opaque black
transparent to translucent yellow, may show chatoyancy
Andradite includes three varieties:
Colophonite : a historical variety found in the Scandinavian islands, brownish or reddish in color, often opaque or translucent.[6 ] : 61
Demantoid : Vivid green in color, one of the most valuable and rare stones in the gemological world.[7 ]
Melanite : Black in color due to limited substitution of titanium for iron. Also known as "titanian andradite". Forms a solid solution with morimotoite and schorlomite depending on titanium and iron content.[8 ]
Topazolite : Yellow-green in color and sometimes of high enough quality to be cut into a faceted gemstone , it is rarer than demantoid.[7 ]
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
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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 Mountains of Russia , Arizona and California and in Dnipropetrovsk Oblast in Ukraine .
Like the other garnets, andradite crystallizes in the cubic space group [[Ia 3 d ]], 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 (T N =11 K[11 ] ).
See also
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References
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^ 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.
External links
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Media related to Andradite at Wikimedia Commons
R e t r i e v e d f r o m " https://en.wikipedia.org/w/index.php?title=Andradite&oldid=1222194696 "
L a s t e d i t e d o n 4 M a y 2 0 2 4 , a t 1 4 : 0 9
L a n g u a g e s
● ا ل ع ر ب ي ة
● A s t u r i a n u
● A z ə r b a y c a n c a
● Б е л а р у с к а я
● Б е л а р у с к а я ( т а р а ш к е в і ц а )
● Б ъ л г а р с к и
● C a t a l à
● Č e š t i n a
● D e u t s c h
● Ε λ λ η ν ι κ ά
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● ف ا ر س ی
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● I t a l i a n o
● ע ב ר י ת
● Қ а з а қ ш а
● L i e t u v i ų
● M a g y a r
● N e d e r l a n d s
● 日 本 語
● N o r s k n y n o r s k
● O ʻ z b e k c h a / ў з б е к ч а
● P o l s k i
● P o r t u g u ê s
● Р у с с к и й
● S l o v e n š č i n a
● S v e n s k a
● Т о ҷ и к ӣ
● У к р а ї н с ь к а
● 中 文
● T h i s p a g e w a s l a s t e d i t e d o n 4 M a y 2 0 2 4 , a t 1 4 : 0 9 ( U T C ) .
● C o n t e n t i s a v a i l a b l e u n d e r C C B Y - S A 4 . 0 u n l e s s o t h e r w i s e n o t e d .
● P r i v a c y p o l i c y
● A b o u t W i k i p e d i a
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