Cordierite

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Cordierite
Specific gravity
2.57–2.66
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[2][3][4][5]

Cordierite (

polymorph exists, indialite, which is isostructural with beryl and has a random distribution of Al in the (Si,Al)6O18 rings.[4]
Cordierite is also synthesized and used in high temperature applications such as catalytic converters and pizza stones.

Crystal structure of Cordierite. GreenMg or Fe, blueO, yellowSi and Al.

Name and discovery

Cordierite, which was discovered in 1813, in specimens from

Níjar, Almería, Spain, is named after the French geologist Louis Cordier (1777–1861).[3]

Occurrence

Cordierite typically occurs in contact or regional

orthopyroxene. Other associated minerals include garnet (cordierite-garnet-sillimanite gneisses) and anthophyllite.[5][6] Cordierite also occurs in some granites, pegmatites, and norites in gabbroic magmas. Alteration products include mica, chlorite, and talc. Cordierite occurs, for example, 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 along one axis. This prevents thermal shock cracking from taking place when the catalytic converter is used.[7]

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.[8] 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.[9]

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 (4,800 g), and was discovered in Wyoming, US.[10]

  • Left: rough specimen showing dichroism; right: cut stone
    Left: rough specimen showing dichroism; right: cut stone
  • Facet cut iolite gemstone
    Facet cut iolite gemstone
  • Pleochroism of cordierite
    Pleochroism of cordierite

Another name for blue iolite is steinheilite, after Fabian Steinheil, the Russian military governor of Finland who observed that it was a different mineral from quartz.[11] Praseolite is another iolite variety which results from heat treatment. It should not be confused with prasiolite.[12]

See also

References

External links