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pseudosymmetry

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Journal Article
Published: 01 April 2009
American Mineralogist (2009) 94 (4): 609–615.
... pseudosymmetry, the structure is monoclinic (space group C 2) with a = 26.0388(10), b = 15.0651(8), c = 15.5361(8) Å, β = 90.48(1)°, and V = 6094.2(5) Å 3 . The refinement of an anisotropic model led to an R index of 0.0656 for 7143 observed reflections [ I > 2σ( I )] and 0.0759 for all 17 447 independent...
FIGURES
Journal Article
Published: 01 July 2005
American Mineralogist (2005) 90 (7): 1108–1114.
...Paola Bonazzi; Giulio I. Lampronti; Luca Bindi; Stefano Zanardi Abstract The crystal structure of the rare mineral wakabayashilite was solved by direct methods using intensity data collected from a twinned crystal. This study revealed that, in spite of the strong hexagonal pseudosymmetry...
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Journal Article
Published: 01 April 1975
American Mineralogist (1975) 60 (3-4): 175–187.
Journal Article
Published: 01 April 1975
American Mineralogist (1975) 60 (3-4): 273–279.
..., B 2 O 4 (OH). Each octahedral chain has a strong twofold screw pseudosymmetry parallel to the c axis. The pseudosymmetry is such that the chain is nearly perfectly transformed by the screw operations into itself with average atomic displacement of only 0.056(4)Å. This situation theoretically permits...
Image
Published: 01 March 2000
Fig. 7. (a) The M1B-octahedron in pseudosymmetry s d . (b) Schematic energy level schemes for Fe 2+ in octahedra of descending symmetry from O h to C 1 showing the splitting of the 5 T 2g groundstate and the 5 E g excited state of the distorted site and the possible electronic transitions.
Journal Article
Published: 01 October 1972
American Mineralogist (1972) 57 (9-10): 1355–1374.
... is good parallel to {100}. The atomic structure is an extreme example of dense-packing where both O 2- and Ca 2+ ions comprise the dense-packed layers. The [MgO 6 ] octahedra are linked at every corner by [SiO 4 ] tetrahedra, defining a “pinwheel” of 3 m point pseudosymmetry. The pin wheels link...
Journal Article
Published: 01 December 2008
The Canadian Mineralogist (2008) 46 (6): 1511–1526.
... to the pronounced pseudosymmetry, indicates preference for an ordered pattern where Al and Si are distributed on alternating tetrahedra [ d Si–O/ d Al–O = 1.628(1)/1.719(1) Å], so that every SiO 4 tetrahedron is coordinated to four AlO 4 tetrahedra and vice versa . The alternating distribution was independently...
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Journal Article
Published: 01 December 1996
American Mineralogist (1996) 81 (11-12): 1494–1500.
...Paola Bonazzi; Fiorenzo Mazzi Abstract The crystal structure of bottinoite, Ni(H 2 O) 6 [Sb(OH) 6 ] 2 , was determined from a twinned crystal. This study revealed that the strong 3 1 m pseudosymmetry shown by all the natural and synthetic crystals examined results from {10 1 0} twinning...
Journal Article
Published: 01 October 1995
American Mineralogist (1995) 80 (9-10): 1054–1058.
...P. Bonazzi; D. Borrini; F. Mazzi; F. Olmi Abstract The crystal structure of synthetic pääkkönenite, Sb 2.07 As 0.93 S 2.00 , was determined. This study revealed that, in spite of the strong orthorhombic pseudosymmetry shown by Weissenberg photographs, the structure is monoclinic (space group C 2/ m...
Journal Article
Published: 01 October 1974
American Mineralogist (1974) 59 (9-10): 1005–1015.
... on the side withprojecting rings. A pseudosymmetry is dominant in the structure; the two halves of the polyanion as well as two Na atoms are quasi-equivalent. Two of the Na atoms and the hydrogen bonding arrangement do not follow the pseudosymmetry. 1 Paper presented at the XXVII Congress...
Journal Article
Published: 11 April 2023
Mineralogical Magazine (2023) 87 (2): 225–232.
... crystal systems but showing a pseudosymmetry should show the prefix ‘pseudo-’. (iii) Polymorphs with the same crystal system but different space groups are distinguished by the prefix ‘para-’. If three or more polymorphs show the same crystal system but different space groups, the space group notation may...
FIGURES
Journal Article
Published: 01 February 2015
Mineralogical Magazine (2015) 79 (1): 191–203.
... , a ≈ 14.1, b ≈ 14.2, c ≈ 9.9 Å) and PHI ( P 2 1 / m , a ≈ 9.9, b ≈ 14.3, c ≈ 8.7 Å, β = 124.8°) frameworks of similar composition are assembled from identical tetrahedral units, though with a different connectivity. Coherent intergrowth and twinning of the two frameworks lead to P 4 2 / mnm pseudosymmetry...
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Journal Article
Published: 01 December 2006
The Canadian Mineralogist (2006) 44 (6): 1499–1512.
... is a desymmetrized OD structure with profuse twinning. The two types of layers present possess layer symmetries p 1̅ and b 2/ m 11, respectively. These layers respectively have a pseudoperiodicity equal to a /2 and a set of elements of pseudosymmetry which together cause a disorder process. Abstract Nous avons...
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Journal Article
Published: 01 May 2006
European Journal of Mineralogy (2006) 18 (3): 337–344.
... pseudosymmetry mm 2, which is usually adopted for M2 in silicate olivines. The energy difference, δ̄ e , between I. and II. represents the low-symmetry splitting of the excited state 5 E g of octahedral Fe 2+ under m3m. Polarization-averaged energies of the above transition I. and of δ̄ e increase with iron...
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Journal Article
Published: 01 October 1996
The Canadian Mineralogist (1996) 34 (5): 1071–1088.
... of stereochemical and bond-valence arguments. The structure displays strong Pbca pseudosymmetry, especially among the U atoms. The lower symmetry is primarily due to H-bond interactions between interlayer H 2 O groups and O(uranyl) atoms of the structural sheet. © 1996 Mineralogical Association of Canada 1996...
Journal Article
Published: 01 February 1995
The Canadian Mineralogist (1995) 33 (1): 67–75.
..., and on prehnite and epidote coexisting with pumpellyite. Spectroscopic data for prehnite, presented for the first time, are discussed in light of the pseudosymmetry of its structure. The data clearly show the prevailing role of Fe (super 3+) in the crystal chemistry of the paragenetically associated Ca-silicates...
Journal Article
Published: 01 February 1993
American Mineralogist (1993) 78 (1-2): 8–15.
... determined. They are interpreted in terms of crystal field theory using the strong field scheme. Spin-orbit coupling and fourth-order terms were included in the calculation. For Fe 2+ at M2, a pseudosymmetry of mm 2 was assumed. Using the covalency factor α 2 , z e 2 〈 r 2 〉, and z e 2 〈 r 4 〉 as adjustable...
Journal Article
Published: 01 October 1980
American Mineralogist (1980) 65 (9-10): 931–935.
... is similar to that found in close-packed structures. A marked pseudosymmetry (towards the centric group Pcan ) is present in the Sb–O sheet. Copyright © 1980 by the Mineralogical Society of America 1980 ...
Journal Article
Published: 01 December 1979
American Mineralogist (1979) 64 (11-12): 1248–1254.
... are: a = 8.012(2), b = 15.956(4), c = 6.801(2) A , β = 96.60(3)°; Z = 8. A strong P 2 1 / n pseudosymmetry appears in the structure, yet the average pseudo-center is slightly shifted from the correct position 1/4, 0, 1/4 in space group P 2 1 / n . The structure is built up by (010) layers of AsO 4 and MnO 6...
Journal Article
Published: 01 February 1979
American Mineralogist (1979) 64 (1-2): 202–210.
...). The structure consists of tetrahedral layers parallel to (001), superposed at intervals of c /2 and connected by cation polyhedra (RE,Na,Ca-antiprisms and Fe,Mn-octahedra). The {110} twinning, always present and responsible for the tetragonal pseudosymmetry, is explained on structural grounds. The structure...