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albite

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albite (ăl`bīt): see feldspar feldspar (fĕl`spär, fĕld`–) or felspar
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albite

Common feldspar mineral, a sodium aluminosilicate (NaAlSi3O8) that occurs most widely in pegmatites and acid igneous rocks such as granites. It may also be found in low-grade metamorphic rocks (those formed under relatively low temperature and pressure conditions) and in certain sedimentary rocks. Albite usually forms brittle, glassy crystals that may be colourless, white, yellow, pink, green, or black. It is used in the manufacture of glass and ceramics, but its primary geologic importance is as a rock-forming mineral.


albite [′al‚bīt]
(mineralogy)
NaAlSi3O8A colorless or milky-white variety of plagioclase of the feldspar group found in granite and various igneous and metamorphic rocks. Also known as sodaclase; sodium feldspar; white feldspar; white schorl.


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The "black shale" category is typified by the Colombian deposits where emerald occurs in calcite + dolomite + pyrite [+ or -] albite veins in black shales and related rocks.
8]) that show continuous solid solution from albite to anorthite, with CaAl replacing NaSi as the series progresses.
As to the rarity of sodium in meteorites, they do contain traces of albite, a feldspar which contains sodium.
 
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