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Anorthite

Anorthite is one of the plagioclase feldspars, an important group of minerals abundant in the Earth's crust. Anorthite's chemical formula is CaAl2Si2O8.

Table of contents
1 Mineralogy
2 Occurrence
3 Details
4 See also
5 External link

    Mineralogy  

Anorthite is the calcium-rich endmember of the plagioclase system, the other endmember being albite[?] (sodium-rich). The range of intermediate compositions have varying ratios of calcium and sodium ions.

    Occurrence 

Anorthite occurs in igneous and metamorphic[?] rocks. Its type localities[?] are Monte Somma and Valle di Fassa, Italy,

    Details 

Crystallographic systemTriclinic
ColoursNormally colourless or white, colourless in thin section.
LustreVitreous
Hardness6-6.5
Refractive index 1.51
Cleavage3: 1 perfect, 1 good, 1 poor
TwinningMultiple lamellar and Carlsbad twins[?]
PleochroismYellow to dark green to transparent to opaque

 

     See also  

     External link  

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