Albite - WikipediaAlbite is a plagioclase feldspar mineral. It is the sodium endmember of the plagioclase solid solution series. As such it represents a plagioclase with less than 10% anorthite content. The pure albite endmember has the formula NaAlSi3O8. It is a tectosilicate. Its color is usually pure white, hence its name from Latin albus.Albite: Albite mineral information and data. - MindatFeldspar Group . Na-rich end member of the Albite-Anorthite Series . Low- and high-temperature structural modifications exist ('low albite' and 'high albite'), with ordered and disordered Al-Si distribution, respectively.
Feldspar | Minerals Education CoalitionThe minerals included in this group are the orthoclase, microcline and plagioclase feldspars. . Feldspar is mined from large granite bodies (called plutons by geologists), from pegmatites (formed when the last fluid stages of a crystallizing granite becomes concentrated in small liquid and vapor-rich pockets that allow the.mineral albite and where it mined,University of Minnesota's Mineral Pages: Plagioclase FeldsparThis name reflects the minerals' abundance, as most crystalline material found in the field is feldspar. The plagioclase feldspar subgroup consists of a continuous mineral series that is arbitrarily subdivided into six mineral categories whose composition varies from being relatively pure sodium aluminum silicate (albite) to a.
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