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Krivovichev, S. V., Yakovenchuk, V. N., Zhitova, E. S., Zolotarev, A. A., Pakhomovsky, Y. A., Ivanyuk, G. Yu. (2010) Crystal chemistry of natural layered double hydroxides. I. Quintinite-2H-3c from the Kovdor alkaline massif, Kola peninsula, Russia. Mineralogical Magazine, 74 (5) 821-832 doi:10.1180/minmag.2010.074.5.821

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Reference TypeJournal (article/letter/editorial)
TitleCrystal chemistry of natural layered double hydroxides. I. Quintinite-2H-3c from the Kovdor alkaline massif, Kola peninsula, Russia
JournalMineralogical Magazine
AuthorsKrivovichev, S. V.Author
Yakovenchuk, V. N.Author
Zhitova, E. S.Author
Zolotarev, A. A.Author
Pakhomovsky, Y. A.Author
Ivanyuk, G. Yu.Author
Year2010 (October)Volume74
Issue5
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2010.074.5.821Search in ResearchGate
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Mindat Ref. ID244104Long-form Identifiermindat:1:5:244104:1
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Full ReferenceKrivovichev, S. V., Yakovenchuk, V. N., Zhitova, E. S., Zolotarev, A. A., Pakhomovsky, Y. A., Ivanyuk, G. Yu. (2010) Crystal chemistry of natural layered double hydroxides. I. Quintinite-2H-3c from the Kovdor alkaline massif, Kola peninsula, Russia. Mineralogical Magazine, 74 (5) 821-832 doi:10.1180/minmag.2010.074.5.821
Plain TextKrivovichev, S. V., Yakovenchuk, V. N., Zhitova, E. S., Zolotarev, A. A., Pakhomovsky, Y. A., Ivanyuk, G. Yu. (2010) Crystal chemistry of natural layered double hydroxides. I. Quintinite-2H-3c from the Kovdor alkaline massif, Kola peninsula, Russia. Mineralogical Magazine, 74 (5) 821-832 doi:10.1180/minmag.2010.074.5.821
Abstract/NotesThe crystal structure of quintinite-2H-3c, [Mg4Al2(OH)12](CO3)(H2O)3, from the Kovdor alkaline massif, Kola peninsula, Russia, was solved by direct methods and refined to an agreement index (R1) of 0.055 for 484 unique reflections with |Fo| ≥ 4σF. The mineral is rhombohedral, R32, a = 5.2745(7), c = 45.36(1) Å. The diffraction pattern of the crystal has strong and sharp Bragg reflections having h–k = 3n and l = 3n and lines of weak superstructure reflections extended parallel to c* and centred at h–k ≠ 3n. The structure contains six layers within the unit cell with the layer stacking sequence of …AC=CA=AC=CA=AC=CA… The Mg and Al atoms are ordered in metal hydroxide layers to form a honeycomb superstructure. The full superstructure is formed by the combination of two-layer stacking sequence and Mg-Al ordering. This is the first time that a long-range superstructure in carbonate-bearing layered double hydroxide (LDH) has been observed. Taking into account Mg-Al ordering, the unique layer sequence can be written as …=Ab1C=Cb1A=Ab2C=Cb2A=Ab3C=Cb3A=… The use of an additional suffix is proposed in order to distinguish between LDH polytypes having the same general stacking sequence but with different c parameters compared with the ‘standard’ polytype. According to this notation, the quintinite studied here can be described as quintinite-2H-3c or quintinite-2H-3c[6R], indicating the real symmetry.

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