Cordierite
| Cordierite | |
|---|---|
Cordierite from Italy
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| General | |
| Category | Silicate mineral |
| Formula (repeating unit) |
(Mg,Fe)2Al4Si5O18 |
| Strunz classification | 09.CJ.10 |
| Dana classification | 61.02.01.01 Cordierite group |
| Crystal symmetry | 2/m 2/m 2/m Orthorhombic - Dipyramidal |
| Unit cell | a = 17.079 Å, b = 9.730 Å, c = 9.356 Å; Z = 4 |
| Identification | |
| Color | Blue, smoky blue, bluish violet; greenish, yellowish brown, gray; colorless to very pale blue in thin section |
| Crystal habit | Pseudo-hexagonal prismatic twins, as imbedded grains, and massive |
| Crystal system | Orthorhombic - Dipyramidal Space Group: C ccm |
| Twinning | Common on {110}, {130}, simple, lamellar, cyclical |
| Cleavage | Fair on {100}, poor on {001} and {010} |
| Fracture | Subconchoidal |
| Tenacity | Brittle |
| Mohs scale hardness | 7 - 7.5 |
| Luster | Greasy or vitreous |
| Streak | White |
| Specific gravity | 2.57 - 2.66 |
| Optical properties | Usually optically (-), sometimes (+); 2V = 0-90° |
| Refractive index | nα = 1.527 - 1.560 nβ = 1.532 - 1.574 nγ = 1.538 - 1.578 Indices increase with Fe content. |
| Pleochroism | X = pale yellow, green; Y = violet, blue-violet; Z = pale blue |
| Fusibility | on thin edges |
| Diagnostic features | Resembles quartz can be distinguished by pleochroism. Can be distinguished from corundum by its lower hardness |
| References | [1][2][3][4] |
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Contents
Name and discovery
Cordierite, which was discovered in 1813, is named after the French geologist Louis Cordier (1777–1861).[2]Occurrence
Cordierite typically occurs in contact or regional metamorphism of argillaceous rocks. It is especially common in hornfels produced by contact metamorphism of pelitic rocks. Two common metamorphic mineral assemblages include sillimanite-cordierite-spinel and cordierite-spinel-plagioclase-orthopyroxene. Other associated minerals include garnet (cordierite-garnet-sillimanite gneisses) and anthophyllite.[4][5] Cordierite also occurs in some granites, pegmatites, and norites in gabbroic magmas. Alteration products include mica, chlorite, and talc. Cordierite occurs in the granite contact zone at Geevor Tin Mine in Cornwall.Commercial use
Catalytic converters are commonly made from ceramics containing a large proportion of synthetic cordierite. The manufacturing process deliberately aligns the cordierite crystals to make use of the very low thermal expansion seen for one axis. This prevents thermal shock cracking from taking place when the catalytic converter is used.[6]Gem variety
As the transparent variety iolite, it is often used as a gemstone. The name "iolite" comes from the Greek word for violet. Another old name is dichroite, a Greek word meaning "two-colored rock", a reference to cordierite's strong pleochroism. It has also been called "water-sapphire" and "Vikings' Compass" because of its usefulness in determining the direction of the sun on overcast days, the Vikings having used it for this purpose.[7] This works by determining the direction of polarization of the sky overhead. Light scattered by air molecules is polarized, and the direction of the polarization is at right angles to a line to the sun, even when the sun's disk itself is obscured by dense fog or lies just below the horizon.[8]Gem quality iolite varies in color from sapphire blue to blue violet to yellowish gray to light blue as the light angle changes. Iolite is sometimes used as an inexpensive substitute for sapphire. It is much softer than sapphires and is abundantly found in Australia (Northern Territory), Brazil, Burma, Canada (Yellowknife area of the Northwest Territories), India, Madagascar, Namibia, Sri Lanka, Tanzania and the United States (Connecticut). The largest iolite crystal found weighed more than 24,000 carats, and was discovered in Wyoming, US.[9]
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Left: rough specimen showing dichroism; right: cut stone
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Facet cut Iolite gemstone
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Pleochroism of Cordierite
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