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European Journal of Mineralogy; October/November; v. 21; no. 5; p. 1061-1071; DOI: 10.1127/0935-1221/2009/0021-1957
© 2009 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Crystal chemistry and nomenclature of the lovozerite group

Igor V. Pekov1,*, Sergey V. Krivovichev2, Andrey A. Zolotarev2, Viktor N. Yakovenchuk3, Thomas Armbruster4 and Yakov A. Pakhomovsky3

1 Faculty of Geology, Moscow State University, Vorobievy Gory, 119992 Moscow, Russia
2 Department of Crystallography, Faculty of Geology, St. Petersburg State University, University emb. 7/9, 199034 St. Petersburg, Russia
3 Geological Institute of Kola Science Center of Russian Academy of Sciences, Fersman str. 14, 184209 Apatity, Russia
4 Mineralogical Crystallography, Institute of Geological Sciences, University of Bern, Freiestr.3, 3012 Bern, Switzerland

* Corresponding author, e-mail: igorpekov{at}mail.ru

The paper summarizes crystal–chemical data and describes the IMA-accepted nomenclature of lovozerite-group minerals (LGM). The lovozerite group includes nine zeolite-like cyclosilicates with the general formula A3B3C2MSi6O12O6x(OH)x·nH2O, with species-defining M = Zr, Ti, Fe3+, Ca; C = Ca, Mn2+, Na, {square}; A = Na, Ca; B = Na, {square};0 ≤ x ≤ 6; n = 0–1. Their structures are based upon a heteropolyhedral framework consisting of rings of Si-centred tetrahedra and M-centred octahedra forming a 3D system of channels that host A, B, and C cations. The structures can be also considered as based upon pseudocubic modules centred at the midpoint of the Si tetrahedral ring. The M, A, and B cations are located at the borders of the module, whereas C cations are inside the module. The modules are stacked in three different arrangements in LGM allowing distinction of three subgroups: (1) zirsinalite–lovozerite subgroup (includes cation-saturated combeite, kapustinite, kazakovite and zirsinalite, and cation-deficient litvinskite, lovozerite and tisinalite), (2) koashvite subgroup (incl. koashvite) and (3) imandrite subgroup (incl. imandrite). The nature of cation-deficient LGM is discussed. The calculation scheme for empirical formulae of LGM and the criteria of definition of a mineral species (end-members) in the group are given.

Key-words: lovozerite group, cyclosilicate, combeite, imandrite, kapustinite, kazakovite, koashvite, litvinskite, lovozerite, tisinalite, zirsinalite, crystal structure, nomenclature of minerals.







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