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Unit-cell intergrowth of pyrochlore and hexagonal tungsten bronze structures in secondary tungsten minerals

Identifieur interne : 009B17 ( Main/Exploration ); précédent : 009B16; suivant : 009B18

Unit-cell intergrowth of pyrochlore and hexagonal tungsten bronze structures in secondary tungsten minerals

Auteurs : Ian E. Grey [Australie] ; William D. Birch [Australie] ; Catherine Bougerol [France] ; Stuart J. Mills [Australie]

Source :

RBID : Pascal:07-0287176

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English descriptors

Abstract

Structural relations between secondary tungsten minerals with general composition Ax[(W,Fe)(O,OH)3]yH2O are described. Phyllotungstite (A = predominantly Ca) is hexagonal, a = 7.31(3)Å, c = 19.55(1)Å, space group P63/mmc. Pittongite, a new secondary tungsten mineral from a wolframite deposit near Pittong in Victoria, southeastern Australia (A = predominantly Na) is hexagonal, a = 7.286(1)Å, c = 50.49(1)Å, space group P-6m2. The structures of both minerals can be described as unit-cell scale intergrowths of (111)py pyrochlore slabs with pairs of hexagonal tungsten bronze (HTB) layers. In phyllotungstite, the (111)py blocks have the same thickness, 6 Å, whereas pittongite contains pyrochlore blocks of two different thicknesses, 6 and 12 Å. The structures can alternatively be described in terms of chemical twinning of the pyrochlore structure on (111)py oxygen planes. At the chemical twin planes, pairs of HTB layers are corner connected as in hexagonal WO3.


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Le document en format XML

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<name sortKey="Grey, Ian E" sort="Grey, Ian E" uniqKey="Grey I" first="Ian E." last="Grey">Ian E. Grey</name>
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<s1>CSIRO Minerals, Box 312</s1>
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<sZ>4 aut.</sZ>
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<country>Australie</country>
<wicri:noRegion>Clayton South, Vic. 3169</wicri:noRegion>
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<title xml:lang="en" level="a">Unit-cell intergrowth of pyrochlore and hexagonal tungsten bronze structures in secondary tungsten minerals</title>
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<name sortKey="Grey, Ian E" sort="Grey, Ian E" uniqKey="Grey I" first="Ian E." last="Grey">Ian E. Grey</name>
<affiliation wicri:level="1">
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<s1>CSIRO Minerals, Box 312</s1>
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<s3>AUS</s3>
<sZ>1 aut.</sZ>
<sZ>4 aut.</sZ>
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<country>Australie</country>
<wicri:noRegion>Clayton South, Vic. 3169</wicri:noRegion>
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<name sortKey="Birch, William D" sort="Birch, William D" uniqKey="Birch W" first="William D." last="Birch">William D. Birch</name>
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<name sortKey="Bougerol, Catherine" sort="Bougerol, Catherine" uniqKey="Bougerol C" first="Catherine" last="Bougerol">Catherine Bougerol</name>
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<country>France</country>
<wicri:noRegion>38054 Grenoble</wicri:noRegion>
<placeName>
<settlement type="city">Grenoble</settlement>
<region type="region" nuts="2">Auvergne-Rhône-Alpes</region>
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<name sortKey="Mills, Stuart J" sort="Mills, Stuart J" uniqKey="Mills S" first="Stuart J." last="Mills">Stuart J. Mills</name>
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<s1>CSIRO Minerals, Box 312</s1>
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<s3>AUS</s3>
<sZ>1 aut.</sZ>
<sZ>4 aut.</sZ>
</inist:fA14>
<country>Australie</country>
<wicri:noRegion>Clayton South, Vic. 3169</wicri:noRegion>
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<country>Australie</country>
<wicri:noRegion>Melbourne, Vic. 3001</wicri:noRegion>
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<title level="j" type="main">Journal of solid state chemistry : (Print)</title>
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<keywords scheme="KwdEn" xml:lang="en">
<term>Actinides</term>
<term>Bronze type compound</term>
<term>Cellular structure</term>
<term>Crystal defects</term>
<term>Crystal twin</term>
<term>Hexagonal lattices</term>
<term>Inorganic compounds</term>
<term>Intergrowth</term>
<term>Iron</term>
<term>New mineral</term>
<term>Pyrochlore</term>
<term>Pyrochlore type compound</term>
<term>Size effect</term>
<term>Space groups</term>
<term>Thickness</term>
<term>Transition element compounds</term>
<term>Transition elements</term>
<term>Tungsten bronze</term>
<term>Tungsten oxides</term>
<term>Twinning</term>
<term>Unit cell</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Maille cristalline</term>
<term>Intercroissance</term>
<term>Minéral nouveau</term>
<term>Fer</term>
<term>Actinide</term>
<term>Groupe espace</term>
<term>Pyrochlore</term>
<term>Epaisseur</term>
<term>Effet dimensionnel</term>
<term>Maclage</term>
<term>Défaut cristallin</term>
<term>Macle</term>
<term>Structure cellulaire</term>
<term>Métal transition</term>
<term>Pyrochlores</term>
<term>Réseau hexagonal</term>
<term>Bronze tungstène</term>
<term>Bronzes</term>
<term>Tungstène oxyde</term>
<term>Composé minéral</term>
<term>Métal transition composé</term>
<term>W</term>
<term>O W</term>
<term>WO3</term>
<term>6166</term>
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<term>Fer</term>
<term>Composé minéral</term>
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<front>
<div type="abstract" xml:lang="en">Structural relations between secondary tungsten minerals with general composition A
<sub>x</sub>
[(W,Fe)(O,OH)
<sub>3</sub>
]
<sub>y</sub>
H
<sub>2</sub>
O are described. Phyllotungstite (A = predominantly Ca) is hexagonal, a = 7.31(3)Å, c = 19.55(1)Å, space group P6
<sub>3</sub>
/mmc. Pittongite, a new secondary tungsten mineral from a wolframite deposit near Pittong in Victoria, southeastern Australia (A = predominantly Na) is hexagonal, a = 7.286(1)Å, c = 50.49(1)Å, space group P-6m2. The structures of both minerals can be described as unit-cell scale intergrowths of (111)
<sub>py</sub>
pyrochlore slabs with pairs of hexagonal tungsten bronze (HTB) layers. In phyllotungstite, the (111)
<sub>py</sub>
blocks have the same thickness, 6 Å, whereas pittongite contains pyrochlore blocks of two different thicknesses, 6 and 12 Å. The structures can alternatively be described in terms of chemical twinning of the pyrochlore structure on (111)
<sub>py</sub>
oxygen planes. At the chemical twin planes, pairs of HTB layers are corner connected as in hexagonal WO
<sub>3</sub>
.</div>
</front>
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<li>France</li>
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<name sortKey="Birch, William D" sort="Birch, William D" uniqKey="Birch W" first="William D." last="Birch">William D. Birch</name>
<name sortKey="Mills, Stuart J" sort="Mills, Stuart J" uniqKey="Mills S" first="Stuart J." last="Mills">Stuart J. Mills</name>
<name sortKey="Mills, Stuart J" sort="Mills, Stuart J" uniqKey="Mills S" first="Stuart J." last="Mills">Stuart J. Mills</name>
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