- Anorthite
Infobox mineral
name = Anorthite
category = Feldspar mineral
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caption = Anorthite from Japan
formula = CaAl2Si2O8
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color = White, grayish, reddish
habit = Anhedral to subhedral granular
system =Triclinic
twinning = Common
cleavage = Perfect [001] good [010]
fracture = Uneven to concoidal
tenacity = Brittle
mohs = 6
luster = Vitreous
polish =
refractive = nα = 1.573 - 1.577 nβ = 1.580 - 1.585 nγ = 1.585 - 1.590
opticalprop = Biaxial (-), 2V 78° to 83°
birefringence = δ = 0.012 - 0.013
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gravity = 2.72 - 2.75
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diaphaneity = Transparent to translucent
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references = http://www.handbookofmineralogy.org/pdfs/anorthite.pdf Handbook of Mineralogy] [http://www.mindat.org/min-246.html Mindat] http://webmineral.com/data/Anorthite.shtml Webmineral]Anorthite is a compositional variety of
plagioclase feldspar . Plagioclase is an abundantmineral in theEarth 's crust. The formula of pure anorthite is CaAl2Si2O8.Mineralogy
Anorthite is the
calcium -rich endmember of the plagioclasesolid solution series, the other endmember beingalbite , NaAlSi3O8. Anorthite also refers to plagioclase compositions with more than 90molecular percent of the anorthite endmember.Occurrence
Anorthite is a rare compositional variety of plagioclase. It occurs in
mafic igneous. It also occurs ingranulite faciesmetamorphic rock s, in metamorphosedcarbonate rock s andcorundum deposits. Its type localities areMonte Somma andValle di Fassa ,Italy . It was first described in 1823.It also makes up much of the lunar highlands. Anorthite was discovered in samples from
comet Wild 2 , and the mineral is an important constituent ofCa-Al-rich inclusions in rare varieties of chondritic meteorites.See also
*
Feldspar s
*List of minerals
*In-Situ Resource Utilization References
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