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آلبیت

File:Albite_-_Crete_(Kriti)_Island,_Greece.jpg · Wikimedia Commons · See Wikimedia Commons

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آلبیت

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Albite is a plagioclase feldspar mineral. It is the sodium endmember of the plagioclase solid solution series. It represents a plagioclase with less than 10% anorthite content. The pure albite endmember has the formula . It is a tectosilicate. Its color is usually pure white, hence its name from Latin, . It is a common constituent in felsic rocks.

Key facts

Mineral.name
Albite
Mineral.category
Tectosilicate minerals
Mineral.group
Feldspar group
Mineral.series
Plagioclase feldspar series
Mineral.image
Albite - Crete (Kriti) Island, Greece.jpg
Mineral.formula
(ideal endmember) (Na:Ca = 100:0 to 90:10)
Mineral.IMAsymbol
Ab
Mineral.IMAstatus
Grandfathered (1815)
Mineral.strunz
9.FA.35
Mineral.dana
76.1.3.1
Mineral.system
Triclinic
Mineral.class
Pinacoidal ()
Mineral.symmetry
C (no. 2)
Mineral.color
White to gray, blueish, greenish, reddish; may be chatoyant
Mineral.habit
Crystals commonly tabular, divergent aggregates, granular, cleavable massive
Mineral.twinning
Common giving polysynthetic striae on {001} or {010} also contact, simple and multiple
Mineral.cleavage
Perfect on {001}, very good on {010}, imperfect on {110}
Mineral.fracture
Uneven to conchoidal

via Wikipedia infobox

Wikidata facts

Subclass of
plagioclase
Named after
white
Image
Albite2.jpg
Show 11 more facts
solid solution series with
moonstone
Commons category
Albite
mineral fracture
conchoidal fracture
chemical formula
NaAlSi₃O₈
Strunz 8th edition (series ID, updated)
VIII/F.03c
Nickel-Strunz 9th edition (updated 2009)
9.FA.35
streak color
white
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.FA.35
IMA Mineral Symbol
Ab
Sources (4)

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Gallery (4)