Cordierite

Cordierite (mineralogy) or iolite (gemology) is a magnesium iron aluminium cyclosilicate. Iron is almost always present, and a solid solution exists between Mg-rich cordierite and Fe-rich sekaninaite with a series formula: (Mg,Fe)2Al3(Si5AlO18) to (Fe,Mg)2Al3(Si5AlO18). A high-temperature polymorph exists, indialite, which is isostructural with beryl and has a random distribution of Al in the (Si,Al)6O18 rings. Cordierite is also synthesized and used in high temperature applications such as catalytic converters and pizza stones.

Cordierite
General
CategoryCyclosilicate
Formula
(repeating unit)
(Mg,Fe)2Al4Si5O18
IMA symbolCrd
Strunz classification9.CJ.10
Dana classification61.02.01.01
Cordierite group
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupCccm
Unit cella = 17.079 Å,
b = 9.730 Å,
c = 9.356 Å; Z = 4
Identification
ColorBlue, smoky blue, bluish violet; greenish, yellowish brown, gray; colorless to very pale blue in thin section in transmitted light
Crystal habitPseudo-hexagonal prismatic twins, as imbedded grains, and massive
TwinningCommon on {110}, {130}, simple, lamellar, cyclical
CleavageFair on {100}, poor on {001} and {010}
FractureSubconchoidal
TenacityBrittle
Mohs scale hardness7–7.5
LusterGreasy or vitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.57–2.66
Optical propertiesUsually optically (-), sometimes (+); 2V = 0–90°
Refractive indexnα = 1.527 – 1.560 nβ = 1.532 – 1.574 nγ = 1.538 – 1.578 Indices increase with Fe content.
PleochroismX = pale yellow, green; Y = violet, blue-violet; Z = pale blue
Fusibilityon thin edges
Diagnostic featuresResembles quartz, can be distinguished by pleochroism. Can be distinguished from corundum by its lower hardness
References
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