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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Congo Democratic Republic
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Shaba Congo Democratic Republic (1)
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East Africa
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Tanzania (1)
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Southern Africa
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Namibia (2)
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Greenland
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Ilimaussaq (1)
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Russian Arctic (1)
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Asia
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Central Asia
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Kazakhstan
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Far East
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Burma (1)
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China
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Japan
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Kamchatka Russian Federation
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Siberia (2)
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Murmansk Russian Federation
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Southern Europe
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tellurium (1)
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fossils
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Invertebrata
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geochronology methods
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geologic age
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Mesozoic
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upper Precambrian
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metamorphic rocks
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phosphates
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apatite (1)
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silicates
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astrophyllite (1)
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charoite (1)
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prehnite (3)
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omphacite (1)
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orthopyroxene
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protoenstatite (1)
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framework silicates
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plagioclase
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nepheline group
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silica minerals
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quartz (2)
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zeolite group
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orthosilicates
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phenakite group
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zircon group
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sorosilicates
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ring silicates
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sheet silicates
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chlorite group
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clay minerals
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beidellite (2)
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smectite (2)
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cymrite (3)
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illite (2)
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mica group
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annite (1)
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biotite (3)
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phlogopite (2)
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polylithionite (1)
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palygorskite (1)
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pyrophyllite (1)
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serpentine group
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chrysotile (1)
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cronstedtite (1)
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stilpnomelane (1)
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sulfates
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anhydrite (2)
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celestine (1)
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sulfides
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cinnabar (1)
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covellite (1)
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djurleite (2)
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galena (2)
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heazlewoodite (1)
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mackinawite (1)
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pyrite (6)
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realgar (4)
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sulfarsenites
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pearceite (4)
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sulfobismuthites
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berryite (1)
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galenobismutite (1)
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gustavite (1)
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lillianite (3)
-
-
-
uranium minerals (9)
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vanadates (3)
-
-
Primary terms
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absolute age (1)
-
Africa
-
Central Africa
-
Congo Democratic Republic
-
Shaba Congo Democratic Republic (1)
-
-
-
East Africa
-
Tanzania (1)
-
-
Southern Africa
-
Namibia (2)
-
-
-
Arctic region
-
Greenland
-
Ilimaussaq (1)
-
South Greenland (1)
-
-
Russian Arctic (1)
-
-
Asia
-
Central Asia
-
Kazakhstan
-
Kokchetav Kazakhstan
-
Kokchetav Massif (1)
-
-
-
-
Far East
-
Burma (1)
-
China
-
Hebei China
-
Jixian China (1)
-
-
Liaoning China
-
Liaodong Peninsula (1)
-
-
North China Platform (1)
-
-
Japan
-
Sambagawa Belt (1)
-
-
-
Kamchatka Russian Federation
-
Kamchatka Peninsula
-
Tolbachik (1)
-
-
-
Krasnoyarsk Russian Federation
-
Taymyr Dolgan-Nenets Russian Federation
-
Norilsk region (1)
-
-
-
Siberia (2)
-
Verkhoyansk region (2)
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Yakutia Russian Federation
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Udachnaya Pipe (1)
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associations (2)
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Australasia
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Australia
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Western Australia (1)
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biogeography (1)
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boron (2)
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Canada
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Eastern Canada
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Maritime Provinces
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Ontario (1)
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Quebec
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Charlevoix (1)
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Rouville County Quebec
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Mont-Saint-Hilaire Quebec (4)
-
-
-
-
Western Canada
-
Manitoba (1)
-
Yukon Territory
-
Royal Creek (1)
-
-
-
-
carbon
-
C-13/C-12 (1)
-
-
Cenozoic
-
Tertiary
-
Paleogene (1)
-
-
-
clay mineralogy (3)
-
core (1)
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crust (1)
-
crystal chemistry (70)
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crystal growth (24)
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crystal structure (136)
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crystallography (3)
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earthquakes (1)
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education (1)
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electron microscopy (1)
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Europe
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Alps (1)
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Azov region (2)
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Carpathians
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Vrancea Mountains (1)
-
-
Central Europe
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Austria
-
Salzburg State Austria
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Salzburg Austria (1)
-
-
-
Black Forest (1)
-
Czech Republic
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Bohemia
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Kutna Hora Czech Republic (1)
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Pribram Czech Republic (1)
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Fichtelgebirge (1)
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Germany
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Baden-Wurttemberg Germany (1)
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Bavaria Germany (1)
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Freiberg Germany (1)
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Odenwald (2)
-
-
Switzerland
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Valais Switzerland
-
Binnental (2)
-
-
-
-
Murmansk Russian Federation
-
Khibiny Mountains (1)
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Kola Peninsula (3)
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Kovdor Massif (1)
-
Lovozero Massif (3)
-
-
Southern Europe
-
Greece
-
Greek Aegean Islands
-
Cyclades (1)
-
-
Sterea Ellas
-
Attica Greece (2)
-
Laurion Greece (1)
-
-
-
Italy
-
Apennines
-
Apuane Alps (6)
-
-
Campania Italy
-
Monte Somma (1)
-
-
Lombardy Italy (1)
-
Sicily Italy
-
Lipari Islands
-
Vulcano (2)
-
-
-
Tuscany Italy
-
Apuane Alps (6)
-
-
-
Romania
-
Vrancea Mountains (1)
-
-
Yugoslavia (1)
-
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Stavelot-Venn Massif (1)
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Ukraine (1)
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Western Europe
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Ardennes (1)
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Belgium (1)
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France
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Loire-Atlantique France (1)
-
-
Scandinavia
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Finland (1)
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Norway
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Oslo Norway (1)
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Vestfold Norway
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Larvik Norway (2)
-
-
-
-
United Kingdom
-
Great Britain
-
England
-
Somerset England (1)
-
-
-
-
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1-20 OF 184 RESULTS FOR
pseudosymmetry
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Journal Article
Fettelite, [Ag 6 As 2 S 7 ][Ag 10 HgAs 2 S 8 ] from Chañarcillo, Chile: Crystal structure, pseudosymmetry, twinning, and revised chemical formula
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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...
Includes: Supplemental Content
Journal Article
Wakabayashilite, [(As,Sb) 6 S 9 ][As 4 S 5 ]: Crystal structure, pseudosymmetry, twinning, and revised chemical formula
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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...
Journal Article
Cation ordering and pseudosymmetry in layer silicates
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 April 1975
American Mineralogist (1975) 60 (3-4): 175–187.
Journal Article
Szaibelyite, Mg 2 (OH)[B 2 O 4 (OH)]: Crystal structure, pseudosymmetry, and polymorphism
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
(a) The M1B-octahedron in pseudosymmetry s d . (b) Schematic energy level s...
in Synthetic and natural Fe-Mg chloritoid : structural, spectroscopic and thermodynamic studies
> European Journal of Mineralogy
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
Atomic Arrangement of Merwinite, Ca 3 Mg[SiO 4 ] 2 , an Unusual Dense-packed Structure of Geophysical Interest
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
THE STRUCTURE OF “ORTHORHOMBIC” KAlSiO 4 - O1 : EVIDENCE FOR Al–Si ORDER FROM MAS NMR DATA COMBINED WITH RIETVELD REFINEMENT AND ELECTRON MICROSCOPY
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
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...
Journal Article
Bottinoite, Ni(H 2 O) 6 [Sb(OH) 6 ] 2 ; crystal structure, twinning, and hydrogen-bond model
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
Crystal structure and twinning of Sb 2 AsS 2 , the synthetic analogue of pääkkönenite
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
The crystal structure of biringuccite, Na 4 [B 10 O 16 (OH) 2 ]· 2H 2 O
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
CNMNC guidelines for the nomenclature of polymorphs and polysomes
Journal: Mineralogical Magazine
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...
Journal Article
Structural intergrowth of merlinoite/phillipsite and its temperature-dependent dehydration behaviour: a single-crystal X-ray study
Journal: Mineralogical Magazine
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...
Journal Article
THE CRYSTAL STRUCTURE OF DADSONITE
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
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...
Journal Article
Electronic absorption spectra of phosphate minerals with olivine-type structures : I. Members of the triphylite-lithiophilite series, M1[6] Li M2[6] (Fe x 2+ Mn 1-x 2+ )[PO 4 ]
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
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...
Journal Article
The crystal structure of schoepite, [(UO 2 ) 8 O 2 (OH) 12 ](H 2 O) 12
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
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
Spectroscopic data on coexisting prehnite-pumpellyite and epidote-pumpellyite
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
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
Local electronic states of Fe 2+ ions in orthopyroxene
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
The crystal structure of klebelsbergite, Sb 4 O 4 (OH) 2 SO 4
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
Krautite, Mn(H 2 O)(AsO 3 OH): crystal structure, hydrogen bonding and relations with haidingerite and pharmacolite
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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
The crystal structure of semenovite
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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...
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