- Augite
Infobox mineral
name = Augite
category = Silicate mineral
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formula = (Ca,Mg,Fe)SiO3
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color = Pale brown to purplish or greenish brown, also dark grey sometimes
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system =Monoclinic
twinning =
cleavage = {110} good
fracture = uneven
mohs = 5 to 6.5
luster = Vitreous
refractive = α = 1.671 - 1.735, β = 1.672 - 1.741, γ = 1.703 - 1.774
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streak = Greenish-white
gravity = 3.19 - 3.56
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other =Augite is a
mineral described chemically as (Ca,Mg,Fe)SiO3 orcalcium magnesium iron silicate . Thecrystal s are monoclinic and prismatic. Augite has two prominent prismatic cleavages, meeting at angles near 90°.Augite is a
solid solution in thepyroxene group.Diopside andhedenbergite are important endmembers in augite, but augite can also contain significantaluminium ,titanium , andsodium and other elements. The calcium content of augite is limited by a miscibility gap between it andpigeonite andorthopyroxene : when occurring with either of these other pyroxenes, the calcium content of augite is a function of temperature and pressure, but mostly of temperature, and so can be useful in reconstructing temperature histories of rocks. With declining temperature, augite may exsolve lamellae of pigeonite and/or orthopyroxene. There is also a miscibility gap between augite andomphacite , but this gap occurs at lower temperature and is not well understood.It is found in
igneous rock s; for example,gabbro andbasalt . It also occurs in relatively high-temperaturemetamorphic rock s such asmafic granulite .Occasional specimens have a shiny appearance that give rise to the mineral's name, which is from the Greek "augites", meaning "brightness", although ordinary specimens have a dull (dark green, brown or black) finish.
References
* Deer, W. A., Howie, R. A., and Zussman, J. (1992). "An introduction to the rock-forming minerals (2nd ed.)". Harlow: Longman ISBN 0-582-30094-0
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