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anorthite

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anorthite (ănôr`thīt): see feldspar feldspar or felspar , an abundant group of rock-forming minerals which constitute 60% of the earth's crust. Chemically the feldspars are silicates of aluminum, containing sodium, potassium, iron, calcium, or barium or combinations of these
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anorthite

Feldspar mineral, calcium aluminosilicate (CaAl2Si2O8), that occurs as white or grayish, brittle, glassy crystals. Primarily a rock-forming mineral, it is used in the manufacture of glass and ceramics. Anorthite occurs in basic igneous rocks (see acid and basic rocks).


anorthite [ə′nȯr‚thīt]
(mineralogy)
The white, grayish, or reddish calcium-rich end member of the plagioclase feldspar series; composition ranges from Ab10An90to Ab0An100, where Ab = NaAlSi3O8and An = CaAl2Si2O8. Also known as calciclase; calcium feldspar.


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8]) that show continuous solid solution from albite to anorthite, with CaAl replacing NaSi as the series progresses.
25x) PHOTO : CL micrograph of a buildup sample showing anorthite (yellow), corundum (red) and hercynite (black) crystals.
2000), plagioclase (mainly alkalic plagioclase of the anorthite type) appears to be a little more resistant to acid hydrolysis than orthoclase.
 
 
 
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