Difference between revisions of "Andalusite"

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It is associated with [[mica]] schist which increases alkali content in ultimate product and so it has not been exploited economically so far.
 
It is associated with [[mica]] schist which increases alkali content in ultimate product and so it has not been exploited economically so far.
 
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Andalusite is a common regional metamorphic mineral which forms under low pressure and moderate to high temperatures. Called Lapis Crucifer in ancient texts. <br><br>The minerals kyanite and sillimanite are polymorphs of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found.
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Andalusite is a common regional metamorphic mineral which forms under low pressure and moderate to high temperatures. Called [[Lapis Crucifer]] in ancient texts. <br><br>The minerals kyanite and sillimanite are polymorphs of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found.
 
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<b>Full information on this product is in the process of completion.</b>
 
<b>Full information on this product is in the process of completion.</b>
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See also [[Aluminium silicate]]
 
[[Category:Minerals and rocks]]
 
[[Category:Minerals and rocks]]
 
[[Category:Products]]
 
[[Category:Products]]

Revision as of 12:29, 16 August 2012

Infobox on Andalusite
Example of Andalusite
Andalusite.jpg
Facts
Origin
Stowage factor (in m3/t)
Humidity / moisture
Ventilation
Risk factors

Andalusite

Contents

Andalusite is an aluminium nesosilicate mineral with the chemical formula Al2SiO5.

The variety chiastolite commonly contains dark inclusions of carbon or clay which form a checker-board pattern when shown in cross-section. A clear variety first found in Andalusia, Spain can be cut into an interesting gemstone.

Faceted andalusite stones give a play of red, green, and yellow colors that resembles a muted form of iridescence, although the colors are actually the result of unusually strong pleochroism.

It is associated with mica schist which increases alkali content in ultimate product and so it has not been exploited economically so far.

Andalusite is a common regional metamorphic mineral which forms under low pressure and moderate to high temperatures. Called Lapis Crucifer in ancient texts.

The minerals kyanite and sillimanite are polymorphs of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found.

Full information on this product is in the process of completion.

See also Aluminium silicate