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Refinement of the crystal structure of berezanskite, Ti22KLi3(Si12O30)

Published online by Cambridge University Press:  02 January 2018

F. C. Hawthorne ,
E. Sokolova ,
L.A. Pautov ,
A. A. Agakhanov  and
V. Yu. Karpenko
F. C. Hawthorne*
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada
E. Sokolova
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada
L.A. Pautov
Affiliation:
Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskii Prospect 18-2, Moscow 117071 Russia
A. A. Agakhanov
Affiliation:
Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskii Prospect 18-2, Moscow 117071 Russia
V. Yu. Karpenko
Affiliation:
Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskii Prospect 18-2, Moscow 117071 Russia
*
E-mail: frank_hawthorne@umanitoba.ca
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Abstract

Berezanskite, ideally Ti□2KLi3(Si12O30), is hexagonal, space group P6/mcc, a = 9.898(4), c = 14.276(6) Å, V = 1211.2(9) Å3, Z = 2. The crystal structure was refined to an R1 index of 2.08% based on 392 unique observed reflections. Berezanskite is isostructural with milarite, ideally ACa2BoCKT(2)(Be2Al)(T(1)Si12O30)(H2O)0–2. The structural unit is of the form [T(2)3T(1)12O30] with T(1) = Si and T(2) = Li, in which (LiO4) tetrahedra link [Si12O30] six-membered double-rings into a framework. The A, B and C sites occur in the interstices of the framework with the following site populations: A = Ti4+2, <A–O>= 1.938(2) Å; B =□2; C = K, <C–O> = 3.058(2) Å. In the T(2) = Li3 milarite-group minerals, the <C–O> distance is inversely related to the occupancy of the B site.

Keywords

berezanskitemilarite groupDarai-PiozTajikistancrystal structureelectron microprobe analysis
Type
Research Article
Information
Mineralogical Magazine , Volume 80 , Issue 5 , August 2016 , pp. 733 - 737
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2016

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