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Enstatite
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{{short description|Pyroxene: magnesium-iron silicate with MgSiO<sub>3</sub> and FeSiO<sub>3</sub> end-members}} {{for|E-type chondrites|Enstatite chondrite}} {{Infobox mineral | name = Enstatite | category = [[Inosilicate]] | image = Enstatite-202036.jpg | imagesize = 260px | caption = | formula = MgSiO<sub>3</sub> | IMAsymbol = En<ref>{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMAβCNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291β320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}</ref> | molweight = {{chem molar mass|Mg=1|Si=1|O=3}} | strunz = 9.DA.05 | system = [[Orthorhombic]] | class = Dipyramidal (mmm) <br/>[[H-M symbol]]: (2/m 2/m 2/m) | symmetry = ''Pbca'' | unit cell = a = 18.23, b = 8.84 <br/>c = 5.19 [Γ ]; Z = 8 | color = White, grey, green, yellow or brown - colorless in thin section. | habit = Prismatic crystals, commonly lamellar, fibrous, or massive | twinning = Simple and lamellar on [100] | cleavage = Good/distinct on [210] | fracture = Uneven | tenacity = Brittle | mohs = 5 to 6 | luster = Vitreous, pearly on cleavage | refractive = n<sub>Ξ±</sub> = 1.650β1.668; n<sub>Ξ²</sub> = 1.652β1.673; n<sub>Ξ³</sub> = 1.659β1.679 | opticalprop = Biaxial (+) | 2V = 55β90Β° | birefringence = Ξ΄ = 0.009β0.011 | pleochroism = Pink to green pleochroism diagnostic for enstatite, pale green to pale orange perpendicular to pink-green axis | streak = Gray | gravity = 3.2β3.3 | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Translucent to opaque | other = | references = <ref name=HBM>[http://rruff.geo.arizona.edu/doclib/hom/enstatite.pdf Handbook of Mineralogy]</ref><ref name=Mindat>[http://www.mindat.org/min-1384.html Mindat]</ref><ref name=Webmin>[http://www.webmineral.com/data/Enstatite.shtml Webmineral data]</ref> }} '''Enstatite''' is a mineral; the magnesium endmember of the [[pyroxene]] [[silicate mineral]] series enstatite (MgSiO<sub>3</sub>) β ferrosilite (FeSiO<sub>3</sub>). The magnesium rich members of the [[solid solution]] series are common rock-forming [[mineral]]s found in [[igneous]] and [[metamorphic rock|metamorphic]] rocks. The intermediate composition, {{chem|(Mg|,Fe)|Si|O|3}}, has historically been known as [[hypersthene]], although this name has been formally abandoned and replaced by orthopyroxene. When determined [[Petrography|petrographically]] or chemically the composition is given as relative proportions of enstatite (En) and ferrosilite (Fs) (e.g., En<sub>80</sub>Fs<sub>20</sub>).
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