Baratovite | |
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General | |
Category | Mineral |
Formula (repeating unit) | KCa7(Ti,Zr)2Li3Si12O36F2 |
IMA symbol | Btv[1] |
Strunz classification | 9.CJ.25 |
Dana classification | 61.1.4.2 |
Crystal system | Monoclinic |
Crystal class | Prismatic H-M symbol: 2/m |
Space group | C2/c |
Unit cell | 3,185.91 |
Identification | |
Color | White, colorless, pink |
Twinning | Common on {001} |
Cleavage | Perfect on {001} |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 5 - 6 |
Luster | Vitreous, pearly |
Streak | White |
Specific gravity | 2.92 |
Density | 2.92 |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.674 nβ = 1.671 nγ = 1.666 |
Birefringence | 0.008 |
2V angle | 60° |
Dispersion | Strong r > v |
Common impurities | Fe, Nb, Mn, Na |
Other characteristics | Radioactive |
Baratovite is a very rare cyclosilicate mineral named after Rauf Baratovich Baratov from Tajikistan. It was discovered in 1974 at Dara-Pioz glacier, Tajikistan,[2] and was approved by the International Mineralogical Association only a year later in 1975.[3] The glacier gives home to 133 valid species, and is the type locality of 33 minerals, one of which is baratovite.[2]
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