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==Discovery==
==Discovery==
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Taaffe bought a number of [[precious stones]] from a jeweller in October 1945. Upon noticing inconsistencies between the taaffeite and spinels, Taaffe sent some examples to B. W. Anderson of the Laboratory of the [[London Chamber of Commerce]] for identification on 1 November 1945. When Anderson replied on 5 November 1945, he told Taaffe that they were unsure of whether it was a [[spinel]] or something new; he also offered to write it up in ''[[Gemologist]]''.<ref name="Anderson"/>


[[File:Magnesiotaaffeite-2N2S-76500.jpg|thumb|left|upright|Specimen from [[Ratnapura]], Sri Lanka]]
[[File:Magnesiotaaffeite-2N2S-76500.jpg|thumb|left|upright|Specimen from [[Ratnapura]], Sri Lanka]]

Revision as of 13:17, 21 January 2018

Taaffeite
Magnesiotaaffeite-2N’2S (Mg3Al8BeO16)
Allgemein
KategorieOxide minerals
Formula
(repeating unit)
BeMgAl4O8
Strunz classification4.FC.25
Crystal systemHexagonal
Crystal classDihexagonal pyramidal (6mm)
Trigonal dipyramidal (3m)
(magnesiotaaffeite-6N'3S and ferrotaaffeite-6N'3S)
Identification
ColorColorless, greyish violet, violet red, red, greenish, light green, pink violet, mauve
Crystal habitPrismatic, alluvial grains
TwinningBy reflection on (0001)?
CleavageImperfect/fair/absent
FractureConchoidal
Mohs scale hardness8–8.5
LusterVitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.60–3.61
Optical propertiesUniaxial
Refractive indexnω = 1.722, nε = 1.777
Birefringenceδ = 0.055
PleochroismWeak
References[1][2]

Taaffeite (/ˈtɑːft/; BeMgAl4O8) is a mineral, named after its discoverer Richard Taaffe (1898–1967) who found the first sample, a cut and polished gem, in October 1945 in a jeweler's shop in Dublin, Ireland.[3][4] As such, it is the only gemstone to have been initially identified from a faceted stone. Most pieces of the gem, prior to Taaffe, had been misidentified as spinel. For many years afterwards, it was known only in a few samples, and it is still one of the rarest gemstone minerals in the world.[5]

Since 2002, the International Mineralogical Association-approved name for taaffeite as a mineral is magnesiotaaffeite-2N'2S.

Discovery

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Specimen from Ratnapura, Sri Lanka

Properties

In 1951, chemical and X-ray analysis confirmed the principal constituents of taaffeite as beryllium, magnesium and aluminium,[6] making taaffeite the first mineral to contain both beryllium and magnesium as essential components.[1]

The confusion between spinel and taaffeite is understandable as certain structural features are identical in both. Anderson et al.,[7] classified taaffeite as an intermediate mineral between spinel and chrysoberyl.[8] Unlike spinel, taaffeite displays the property of double refraction that allows distinction between these two minerals.

Usage

Because of its rarity, taaffeite is used only as a gemstone.[9]

Formation and occurrence

Taaffeite occurs in carbonate rocks alongside fluorite, mica, spinel and tourmaline. This extremely rare mineral is increasingly found in alluvial deposits in Sri Lanka[10] and southern Tanzania,[1] as well as lower grade taaffeite in limestone sediments in China.[8]

See also

References

  1. ^ a b c Thomas, Arthur (2008) Gemstones: properties, identification and use. New Holland Publishers. p. 74. ISBN 1-84537-602-1
  2. ^ Magnesiotaaffeite, Mindat
  3. ^ Dept. Mineralogy, British Museum, June 7 1951 Taaffeite, a new beryllium mineral, found as a cut gem-stone. Retrieved February 2015
  4. ^ Papers and proceedings of the International Mineralogical Association. General meeting, Mineralogical Society of America, Volume 9, p. 502
  5. ^ Collings, Michael R (2009). Gemlore: An Introduction to Precious and Semi-Precious Stones (2nd Ed). p. 152. Wildside Press LLC. ISBN 1-4344-5702-8
  6. ^ Read, Peter G. (2005). Gemmology. Butterworth-Heinemann. p. 5. ISBN 0-7506-6449-5.
  7. ^ Anderson, B.W., Payne, C.J., and Claringbull, G.F., (1951) Taaffeite, a new beryllium mineral, found as a cut gemstone. Mineralogical Magazine 29, pp. 765–772
  8. ^ a b Institut mineralogii, geokhimii, i kristallokhimii redkikh ėlementov (1966). Geochemistry and mineralogy of rare elements and genetic types of their deposits, Volume 2. Institut mineralogii, geokhimii i kristallokhimii redkikh elementov. (English Version Publisher: Israel Program for Scientific Translations). pp. 77–79.
  9. ^ Amethyst Galleries Inc.
  10. ^ Geological abstracts, Issues 1–7259 (1992). Elsevier/Geo Abstracts, p. 565