Bertrandite | |
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Bertrandite from the Golconda pegmatite, Minas Gerais, Brazil | |
General | |
Category | Sorosilicate |
Formula (repeating unit) | Be4Si2O7(OH)2 |
IMA symbol | Btd |
Strunz classification | 9.BD.05 |
Crystal system | Orthorhombic |
Crystal class | Pyramidal (mm2) H-M symbol: (mm2) |
Space group | Ccm21 |
Unit cell | a = 8.7135(4) Å, b = 15.268(1) Å, c = 4.5683(3) Å; Z = 4 |
Identification | |
Color | Colorless to pale yellow |
Crystal habit | Thin tabular, prismatic to needle-like crystals commonly in radial clusters |
Twinning | Common on {011} or {021} forming heart- or V-shaped twins |
Cleavage | Perfect on {001}; distinct on {100}, {010} and {110} |
Mohs scale hardness | 6–7 |
Luster | Vitreous, pearly on cleavage surfaces |
Diaphaneity | Transparent |
Specific gravity | 2.59–2.60 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.591 nβ = 1.605 nγ = 1.614 |
Birefringence | δ = 0.023 |
2V angle | Measured: 73° to 81° |
References |
Bertrandite is a beryllium sorosilicate hydroxide mineral with composition: Be4Si2O7(OH)2. Bertrandite is a colorless to pale yellow orthorhombic mineral with a hardness of 6–7.
It is commonly found in beryllium rich pegmatites and is in part an alteration of beryl. Bertrandite often occurs as a pseudomorphic replacement of beryl. Associated minerals include beryl, phenakite, herderite, tourmaline, muscovite, fluorite and quartz.
It, with beryl, are ores of beryllium.
It was discovered near Nantes, France in 1883 and named after French mineralogist, Emile Bertrand (1844–1909).
One of the world's largest deposits of bertrandite is Spor Mountain, Thomas Range, Utah which is currently the source of most of the world's beryllium production.
See also
References
- Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ Handbook of Mineralogy
- ^ Bertrandite on Mindat.org
- ^ Bertrandite on Webmineral
- Fact Sheet 2016–3081 (October 2016). "Beryllium—A Critical Mineral Commodity—Resources, Production, and Supply Chain" (Article). usgs.gov/. pubs.usgs.gov: USGS. p. 4. Retrieved 16 May 2017.
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: CS1 maint: numeric names: authors list (link) - Shawe, Daniel (1968). Ridge, John (ed.). Geology of the Spor mountain Beryllium District, Utah, in Ore deposits of the United States, 1933–1967. New York: The American Institute of Mining, Metallurgical, and Petroleum engineers, Inc. pp. 1148–1161.