PLASTIC DEFORMATION OF WADSLEYITE: III. INTERPRETATION OF DISLOCATIONS AND SLIP SYSTEMS

dc.contributor.author	Thurel E.
dc.contributor.author	Douin J.
dc.contributor.author	Cordier P.
dc.date.accessioned	2022-02-13T04:46:05Z
dc.date.available	2022-02-13T04:46:05Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=5092806
dc.identifier.citation	Physics and Chemistry of Minerals, 2003, 30, 5, 271-279
dc.identifier.issn	0342-1791
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35252
dc.description.abstract	Linear anisotropic elasticity has been applied to interpret the dislocation stability and ease of slip in wadsleyite. It is shown that wadsleyite is very isotropic from the elastic point of view. The influence of crystal chemistry and bonding on the choice of the slip plane is discussed. It is shown that slip is predominantly achieved on planes that do not shear Si-O bonds. It is suggested that dissociation of dislocations is essential in determining the ease of slip among the various slip systems.
dc.subject	LINEAR ANISOTROPIC ELASTICITY
dc.subject	DISLOCATION STABILITY
dc.subject	SLIP PLANES
dc.title	PLASTIC DEFORMATION OF WADSLEYITE: III. INTERPRETATION OF DISLOCATIONS AND SLIP SYSTEMS
dc.type	Статья

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