• I.V. Pekov
  • N.V. Zubkova
  • I.I. Chaikovskiy
  • V.O. Yapaskurt
  • N.V. Chukanov
  • D.I. Belakovskiy
  • I.S. Lykova
  • S.N. Britvin
  • D.Y. Pushcharovsky
The new mineral yarzhemskiite, K[B5O7(OH)2]H2O, was found in a halite-sylvite evaporite rock at the Chelkar salt dome, Western Kazakhstan Region, Kazakhstan. It is also associated with carnallite, polyhalite, gypsum, strontioginorite, satimolite and quartz. Yarzhemskiite occurs as separate thick tabular, short prismatic or equant crystals up to 0.5 mm × 0.7 mm × 1 mm and grains having irregular outlines up to 1 mm × 1.5 mm × 2 mm. The mineral is transparent, colourless, with vitreous lustre. It is brittle, the Mohs' hardness is ca 2. Cleavage is perfect on {100}. Dmeas is 2.13(1) and Dcalc is 2.112 g cm-3. Yarzhemskiite is optically biaxial (+), α = 1.484(2), β = 1.508(2), γ = 1.546(2), 2Vmeas = 75(10)° and 2Vcalc = 80°. Chemical composition (wt.%, electron microprobe, H2O was calculated by stoichiometry) is: Na2O 0.01, K2O 17.84, CaO 0.07, B2O3 67.21, H2Ocalc 13.91, total 99.04. The empirical formula based on 10 O atoms per formula unit is K0.98B5.005O7(OH)2H2O. Yarzhemskiite is monoclinic, P21/c,
Original languageEnglish
Pages (from-to)335-342
Number of pages8
JournalMineralogical Magazine
Volume84
Issue number2
DOIs
StatePublished - Apr 2020

ID: 53286769