Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
European Journal of Mineralogy Email Content Delivery
JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

European Journal of Mineralogy; November, December 2001; v. 13; no. 6; p. 1035-1045; DOI: 10.1127/0935-1221/2001/0013-1035
© 2001 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (21)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by NESPOLO, M.
Right arrow Articles by FERRARIS, G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Articles

Effects of the stacking faults on the calculated electron density of mica polytypes — The urovic effect

Massimo NESPOLO1,* and Giovanni FERRARIS2

1 Japan Science and Technology Corporation, National Institute of Research in Inorganic Materials. 1–1 Namiki, Tsukuba-shi, Ibaraki 305–0044, Japan
2 University of Torino, Department of Mineralogical and Petrologic Sciences. Via Valperga Caluso 35, 10125 Torino, Italy

* E-mail: massimo.nespolo{at}nims.go.jp

The occurrence of residues in the Fourier map of OD structures (polytypes in which pairs of building modules are geometrically equivalent) in the positions of the ‘virtual atoms' of the corresponding family structure derives from the presence of stacking faults inside an otherwise ordered (periodic) matrix. These residues are commonly spurious peaks deriving from the refinement of the structure with a single scale factor for both the family and the non-family reflections, which may be instead on a different scale because of the different peak shape and background characterizing the two types of reflections, resulting in broadening and streaking of the non-family reflections. The ‘virtual atoms' occur in the same positions of the atoms corresponding to the stacking faults, but the spurious peaks are in a quantitative relation with them only if the stacking faults diffract coherently. The case of mica polytypes is illustrated also with the aid of examples taken from the literature.

Key-words: OD structures, micas, polytypes, structure refinement, disordered structures, stacking faults..




This article has been cited by other articles:


Home page
American MineralogistHome page
F. Scordari and G. Ventruti
Sideronatrite, Na2Fe(SO4)2(OH){middle dot}3H2O: Crystal structure of the orthorhombic polytype and OD character analysis
American Mineralogist, November 1, 2009; 94(11-12): 1679 - 1686.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
M. Zelenski, A. Garavelli, D. Pinto, F. Vurro, Y. Moelo, L. Bindi, E. Makovicky, and E. Bonaccorsi
Tazieffite, Pb20Cd2(As,Bi)22S50Cl10, a new chloro-sulfosalt from Mutnovsky volcano, Kamchatka Peninsula, Russian Federation
American Mineralogist, October 1, 2009; 94(10): 1312 - 1324.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
D. Pinto, E. Bonaccorsi, T. Balic-Zunic, and E. Makovicky
The crystal structure of vurroite, Pb20Sn2(Bi, As)22S54Cl6: OD-character, polytypism, twinning, and modular description
American Mineralogist, May 1, 2008; 93(5-6): 713 - 727.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
S. Matarrese, E. Schingaro, F. Scordari, F. Stoppa, G. Rosatelli, G. Pedrazzi, and L. Ottolini
Crystal chemistry of phlogopite from Vulture-S. Michele Subsynthem volcanic rocks (Mt. Vulture, Italy) and volcanological implications
American Mineralogist, February 1, 2008; 93(2-3): 426 - 437.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
E. Schingaro, F. Scordari, S. Matarrese, E. Mesto, F. Stoppa, G. Rosatelli, and G. Pedrazzi
Phlogopite from the Ventaruolo subsynthem volcanics (Mt Vulture, Italy): a multi-method study
Mineralogical Magazine, October 1, 2007; 71(5): 519 - 537.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
A. Gianfagna, F. Scordari, S. Mazziotti-Tagliani, G. Ventruti, and L. Ottolini
Fluorophlogopite from Biancavilla (Mt. Etna, Sicily, Italy): Crystal structure and crystal chemistry of a new F-dominant analog of phlogopite
American Mineralogist, October 1, 2007; 92(10): 1601 - 1609.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
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]


Home page
Can MineralHome page
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]


Home page
Clays and Clay MineralsHome page
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]


Home page
Eur J MineralHome page
V. A. DRITS and B. A. SAKHAROV
Potential problems in the interpretation of powder X-ray diffraction patterns from fine-dispersed 2M1 and 3T dioctahedral micas
European Journal of Mineralogy, February 1, 2004; 16(1): 99 - 110.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
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]


Home page
Eur J MineralHome page
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]


Home page
Can MineralHome page
T. Balic-Zunic, D. Topa, and E. Makovicky
THE CRYSTAL STRUCTURE OF EMILITE, Cu10.7Pb10.7Bi21.3S48, THE SECOND 45 A DERIVATIVE OF THE BISMUTHINITE AIKINITE SOLID-SOLUTION SERIES
Can Mineral, February 1, 2002; 40(1): 239 - 245.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
G. FERRARIS, A. GULA, G. IVALDI, M. NESPOLO, E. SOKOLOVA, Y. UVAROVA, and A. P. KHOMYAKOV
First structure determination of an MDO-2O mica polytype associated with a 1M polytype
European Journal of Mineralogy, December 1, 2001; 13(6): 1013 - 1023.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
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]


Home page
Eur J MineralHome page
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
Copyright © 2009 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers