Spessartine

Spessartine, sometimes mistakenly referred to as spessartite,[5] is a nesosilicatemanganese aluminium garnet species, Mn2+3Al2(SiO4)3.[1][2][3][4] The mineral spessartine should not be confused with a type of igneous rock (a lamprophyre) called spessartite.

Spessartine
Spessartine sur quartz fumé.jpg
Spessartine crystals on larger quartz crystals from China
General
CategoryNesosilicate
Garnet group
Formula
(repeating unit)
Mn2+3Al2(SiO4)3
Strunz classification9.AD.25
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H-M symbol: (4/m 3 2/m)
Space groupIa3d
Unit cella = 11.63 Å; Z = 8
Identification
ColorYellow through red
Crystal habitMassive to crystalline
CleavageNone
FractureSub-conchoidal
TenacityBrittle
Mohs scale hardness6.5 – 7.5
LusterVitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity4.19 calculated, 4.12 – 4.32 measured
Optical propertiesIsotropic, often anomalous double refractive
Refractive index1.800
Birefringencenone
DispersionWeak
Absorption spectraBands at 410, 420, 430 nm (or merging to form cutoff below 430 nm; also bands at 460, 480, 520 nm. Possible weak bands at 504 or 573 nm[1]
References[2][3][4]

Spessartine's name is a derivative of Spessart in BavariaGermany, the type locality of the mineral.[2][3] It occurs most often in granite pegmatite[2][3][4] and allied rock types and in certain low-grade metamorphic phyllites. Sources include AustraliaMyanmarIndiaAfghanistanIsraelMadagascarNamibiaNigeriaMozambiqueTanzania and the United States.[1] Spessartine of an orange-yellow has been called Mandarin garnet and is found in Madagascar. Violet-red spessartines are found in rhyolites in Colorado and Maine. In Madagascar, spessartines are exploited either in their bedrock or in alluvium. The orange garnets result from sodium-rich pegmatites. Spessartines are found in bedrock in the highlands in the Sahatany valley. Those in alluvium are generally found in southern Madagascar or in the Maevatanana region.[6][7][8][9][10]

Spessartine forms a solid solution series with the garnet species almandine.[3][4] Well-formed crystals from this series, varying in color from very dark-red to bright yellow-orange, were found in Latinka, Rhodope MountainsKardzhali ProvinceBulgaria.[11] Spessartine, like the other garnets, always occurs as a blend with other species. Gems with high spessartine content tend toward a light orange hue, while almandine prevalence induces red or brownish hues.[12]

ImagesEdit

 


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 Metasyntactic variable, which is released under the 
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