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Stacking variations in cancrinite minerals

Stacking variations in cancrinite minerals TEM reveals (0001) stacking faults and periodic superstructures in cancrinite-related minerals, afghanite and franzinite, which are interpreted as aperiodic or periodic displacements of the hexagonal (Si,Al)6O12 ring units. Franzinite also shows a superstructure when the structure is projected onto the xy plane; satellites occur in the hk0 diffraction patterns. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Crystallographica Section A: Crystal Physics, Diffraction, Theoretical and General Crystallography International Union of Crystallography

Stacking variations in cancrinite minerals

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Stacking variations in cancrinite minerals

Rinaldi, R; Wenk, H.-R
Acta Crystallographica Section A: Crystal Physics, Diffraction, Theoretical and General Crystallography , Volume 35 (5): 825 – Sep 1, 1979

Abstract

TEM reveals (0001) stacking faults and periodic superstructures in cancrinite-related minerals, afghanite and franzinite, which are interpreted as aperiodic or periodic displacements of the hexagonal (Si,Al)6O12 ring units. Franzinite also shows a superstructure when the structure is projected onto the xy plane; satellites occur in the hk0 diffraction patterns.

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Publisher
International Union of Crystallography
Copyright
Copyright (c) 1979 International Union of Crystallography
ISSN
0567-7394
DOI
10.1107/S0567739479001868
Publisher site
See Article on Publisher Site

Abstract

TEM reveals (0001) stacking faults and periodic superstructures in cancrinite-related minerals, afghanite and franzinite, which are interpreted as aperiodic or periodic displacements of the hexagonal (Si,Al)6O12 ring units. Franzinite also shows a superstructure when the structure is projected onto the xy plane; satellites occur in the hk0 diffraction patterns.

Journal

Acta Crystallographica Section A: Crystal Physics, Diffraction, Theoretical and General Crystallography – International Union of Crystallography

Published: Sep 1, 1979

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