Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You or Your Team.

Learn More →

Stacking faults and twins in kyanite, Al2SiO5

Stacking faults and twins in kyanite, Al2SiO5 Two types of twins are frequently found in naturally and experimentally deformed kyanite. Structural models based on periodic shears are proposed to account for these mechanical twins. The structure of kyanite is then regarded as layered, the limits of each layer being easy glide planes for dislocations. The shear plane is (100). The shear vectors are 1/2 001 and 1/2 011. They are suitable for the only known glide system (I00)001. 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 faults and twins in kyanite, Al2SiO5

Download PDF

Stacking faults and twins in kyanite, Al2SiO5

Lefebvre, A; Menard, D
Acta Crystallographica Section A: Crystal Physics, Diffraction, Theoretical and General Crystallography , Volume 37 (1): 80 – Jan 1, 1981

Abstract

Two types of twins are frequently found in naturally and experimentally deformed kyanite. Structural models based on periodic shears are proposed to account for these mechanical twins. The structure of kyanite is then regarded as layered, the limits of each layer being easy glide planes for dislocations. The shear plane is (100). The shear vectors are 1/2 001 and 1/2 011. They are suitable for the only known glide system (I00)001.

Loading next page...
 
/lp/international-union-of-crystallography/stacking-faults-and-twins-in-kyanite-al2sio5-LI2aGKbfkS

References (0)

References for this paper are not available at this time. We will be adding them shortly, thank you for your patience.

Publisher
International Union of Crystallography
Copyright
Copyright (c) 1981 International Union of Crystallography
ISSN
0567-7394
DOI
10.1107/S0567739481000144
Publisher site
See Article on Publisher Site

Abstract

Two types of twins are frequently found in naturally and experimentally deformed kyanite. Structural models based on periodic shears are proposed to account for these mechanical twins. The structure of kyanite is then regarded as layered, the limits of each layer being easy glide planes for dislocations. The shear plane is (100). The shear vectors are 1/2 001 and 1/2 011. They are suitable for the only known glide system (I00)001.

Journal

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

Published: Jan 1, 1981

There are no references for this article.