|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | FEEDBACK/COMMNET | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Articles |
a Dipartimento di Scienze Mineralogiche e Petrologiche, Universitá di Torino, Via Valperga Caluso 35, I-10125 Torino, Italy
b Japan Science and Technology Corporation, National Institute of Research in Inorganic Materials. 11 Namiki, Tsukuba-shi, Ibaraki 3050044, Japan
c Moscow State University, Department of Crystallography, Moscow, Russia
d IMGRE, Russian Academy of Sciences, Moscow, Russia
* E-mail: ferraris{at}dsmp.unito.it
The structure refinement of associated phlogopite-2O and phlogopite-1M from the Khibiny massif (Kola Peninsula, Russia) is reported. Crystal data are:
= 5.2781(5), b = 9.141(1), c = 20.124(4) Å, Ccmm (20); a = 5.305(2), b = 9.199(2), c = 10.232(4) Å, ß = 100.03(2)°, C2/m (1M). Least-squares refinement of single-crystal X-ray diffraction data converged to R1 = 0.034 (2O, 926 independent reflections) and 0.037 (1M, 677 independent reflections). This is the first structure refinement of an MDO (standard) mica-2O: two previous structure reports concerned anandite-2O, which was not a true polytype, having an oP (primitive orthorhombic) lattice not compatible with the C-centred cell common to all mica polytypes. The two phlogopite polytypes show practically the same chemical composition (K0. 95Na0.01) (Mg2.16Fe0.34Ti0.04Mn0.04Li0.40)[Si3.40Al0.60O10][(OH)1.35F0.65] and no cation ordering. Both polytypes are affected by stacking disorder, which broadens the non-family reflections (k
3n). As a consequence, the diffracted intensities of the two types are measured at different scales and large residues in the difference Fourier maps were observed at ± b/3 along [010], [310] and [3
0]. These residues (uroviceffect) disappear by carrying out the refinement with separate scale factors for the two types of reflections. On the basis of structural, morphology and zoning considerations the formation of the two associated polytypes is attributed to chemical oscillation in the crystallization mean.
Key-words: phlogopite-2O, phlogopite-1M, crystal structure, polytypism, stacking disorder..
This article has been cited by other articles:
![]() |
J. Kameda, R. Miyawaki, V. A. Drits, and T. Kogure POLYTYPE AND MORPHOLOGICAL ANALYSES OF GUMBELITE, A FIBROUS Mg-RICH ILLITE Clays and Clay Minerals, October 1, 2007; 55(5): 453 - 466. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. HYBLER Parallel intergrowths in cronstedtite-1T. determination of the degree of disorder European Journal of Mineralogy, April 1, 2006; 18(2): 197 - 205. [Abstract] [Full Text] [PDF] |
||||
![]() |
P. H.J. Mercier, D. G. Rancourt, J.-L. Robert, R. G. Berman, and G. J. Redhammer Fundamental difference between synthetic powder and natural or synthetic single-crystal 1M micas: Geometric homo-octahedral vs. geometric meso-octahedral sheets American Mineralogist, February 1, 2005; 90(2-3): 399 - 410. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. J. Locock, P. C. Burns, and T. M. Flynn DIVALENT TRANSITION METALS AND MAGNESIUM IN STRUCTURES THAT CONTAIN THE AUTUNITE-TYPE SHEET Can Mineral, December 1, 2004; 42(6): 1699 - 1718. [Abstract] [Full Text] [PDF] |
||||
![]() |
S. Durovic, S. Durovic, J. Hybler, and T. Kogure PARALLEL INTERGROWTHS IN CRONSTEDTITE-1T: IMPLICATIONS FOR STRUCTURE REFINEMENT Clays and Clay Minerals, October 1, 2004; 52(5): 613 - 621. [Abstract] [Full Text] [PDF] |
||||
![]() |
S. V. KRIVOVICHEV, T. ARMBRUSTER, V. N. YAKOVENCHUK, Y. A. PAKHOMOVSKY, and Y. P. MEN'SHIKOV Crystal structures of lamprophyllite-2M and lamprophyllite-2O from the Lovozero alkaline massif, Kola peninsula, Russia European Journal of Mineralogy, August 1, 2003; 15(4): 711 - 718. [Abstract] [Full Text] [PDF] |
||||
![]() |
I. V. PEKOV, N. V. CHUKANOV, G. FERRARIS, G. IVALDI, D. Yu. PUSHCHAROVSKY, and A. E. ZADOV Shirokshinite, K(NaMg2)Si4O10F2, a new mica with octahedral Na from Khibiny massif, Kola Peninsula: descriptive data and structural disorder European Journal of Mineralogy, June 1, 2003; 15(3): 447 - 454. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. P. Khomyakov, G. N. Nechelyustov, E. Sokolova, E. Bonaccorsi, S. Merlino, and M. Pasero MEGAKALSILITE, A NEW POLYMORPH OF KAlSiO4 FROM THE KHIBINA ALKALINE MASSIF, KOLA PENINSULA, RUSSIA: MINERAL DESCRIPTION AND CRYSTAL STRUCTURE Can Mineral, June 1, 2002; 40(3): 961 - 970. [Abstract] [Full Text] [PDF] |
||||
![]() |
G. IVALDI, G. FERRARIS, N. CURETTI, and R. COMPAGNONI Coexisting 3T and 2M1 polytypes of phengite from Cima Pal (Val Savenca, western Alps): Chemical and polytypic zoning and structural characterisation European Journal of Mineralogy, December 1, 2001; 13(6): 1025 - 1034. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. NESPOLO and G. FERRARIS Effects of the stacking faults on the calculated electron density of mica polytypes -- The urovic effect European Journal of Mineralogy, December 1, 2001; 13(6): 1035 - 1045. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. PAVESE, G. FERRARIS, V. PISCHEDDA, and F. FAUTH M1-site occupancy in 3T and 2M1 phengites by low temperature neutron powder diffraction: reality or artefact? European Journal of Mineralogy, December 1, 2001; 13(6): 1071 - 1078. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | FEEDBACK/COMMNET | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |