The other end member, Anorthite, contains calcium and no sodium. Yedlin, Neal. Ilmenite Occurrences In Litchfield, Connecticut. Albite. The pure albite endmember has the formula NaAlSi3O8. Gemology [edit | edit source] Gemstone Information. Albite is the sodic end member of both the plagioclase feldspar series and the alkali feldspar series.. The Mineralogical Press, Danbury, Connecticut; Sullivan, Earle C. (1985): History and Minerals of Old Mine Park. Zygadite variety of albite consists of an unusual crystallographic habit: tabular crystals with a steeply acute morphology. Approved, 'Grandfathered' (first described prior to 1959), Image shows birefringence interference colour range (at 30µm thickness). (FRL) - First Recorded Locality for everything else (eg varieties). Quarry), Belley, P, et al. Pyroxene Fe2 EM Fe2Si2O6. Piccoli, G.C. O layers. Hedenbergite. Fys. Anorthite belongs to the Plagioclase Feldspar group, an isomorphous solid solution series. Manchester University Press, U.K. Moore, D.E., Liou, J.G. (1958) The crystal structure of low-temperature and high-temperature albites. High Albite: Stable above 800°C - usually formed in hydrothermal syntheses, has disordered Al-Si arrangement (in contrast to 'low albite'). MacKenzie, W.S., Zussman, J., editors (1974) The Feldspars. (1911) Krystallographische Notizen ueber Albit, Phenakit, und Neptunit: Zeitschr. Second Edition, Revised and Expanded. (2002) I minerali delle Alpi Marittime e Cozie. Pyroxene CaMg EM CaMgSi2O6. (1992) Non-linear temperature dependence of liquid volumes in the system albite-anorthite-diopside. Its color is usually pure white, hence its name from Latin albus. Mineral Data Publishing, Tucson, AZ, 904pp., 2 sub-volumes: 13. Garcia G., Gonzalez C., Bueno A. Kem. High and low forms; both are described in the non-standard space-group C-1 (chosen by convention to facilitate comparison with C-centred monoclinic orthoclase and sanidine). Albite is a plagioclase feldspar mineral. This means that the cut of the rock almost makes a … Armbruster, T., Buergi, H.B., Kunz, M., Gnos, E., Broenniman, S., Lienert, C. (1990): Variation of displacement parameters in structure refinements of low albite. Contributions to Mineralogy and Petrology: 111: 61-73. Albite: An igneous rock composed almost entirely of albite. modified and updated by Barbara Liebman, Boston Mineral Club News, September, 2005, Cambridge, Massachusetts. Its color is usually pure white, hence its name from Latin albus. The cooling history of high-temperature sodium-rich feldspars. Albite Moonstone: Andesine: A plagioclase feldspar with an albite : anorthite molar ratio ranging from 50 : 50 to 70 : 30.: Cleavelandite: Platy albite, generally found in pegmatite. (2007) Minerali del Piemonte e della Valle d'Aosta. (1979) Chessboard-twinned albite from Franciscan metaconglomerates of the Diablo Range, California. The extremes of chemical chemical composition in such isomorphous series are known as end- members Examples: Albite = NaAlSi 3 O 8 = Ab; Orthoclase = KAlSi 3 O 8 = Or, In example 4.2.1., feldspar may be denoted Ab 87 Or 13 Example 4.2.2. Benusa, M.T., Angel, R.J., Ross, N.L. Contributions to Mineralogy and Petrology. Smith, J.V., MacKenzie, W.S. Some excellent examples have come from the Swiss Alps and the Tyrol, Austria. Now regarded as a superflous subdivision of Oligoclase. Pyroxene CaFe EM CaFeSi2O6. Acta Crystallographica: 17: 882-890. Cahoon, James C. (2005) Massachusetts: A Classic Swiss Alpine Cleft Mineral Region. Albite is a plagioclase feldspar mineral. Mineral Name: Albite Chemical Composition: NaAlSi 3 O 8 Color: White, colorless, cream, light yellow, light blue, light green, pale red, light brown, gray Streak: White Hardness: 6-6.5 Cleavage/Fracture: The cleavage is 2 at 90 degrees. Its color is usually pure white, hence its name from Latin albus. 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