1991
DOI: 10.1107/s0108767391006864
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Representation of orientation and disorientation data for cubic, hexagonal, tetragonal and orthorhombic crystals

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Cited by 125 publications
(82 citation statements)
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“…Once the grain positions and orientations have been identified, the locations of all other diffraction spots belonging to each grain can be predicted and, hence, other unpaired, diffraction spots added to the sets. As previously, 3 the orientation of each grain is inferred from the point in the fundamental zone of Rodriguez space, 5 where all projection lines for pole figure inversion of the corresponding grain cross ͑each of the observed scattering vectors defines one of these projection lines in Rodriguez's space͒.…”
Section: Indexing From Friedel Pairsmentioning
confidence: 99%
“…Once the grain positions and orientations have been identified, the locations of all other diffraction spots belonging to each grain can be predicted and, hence, other unpaired, diffraction spots added to the sets. As previously, 3 the orientation of each grain is inferred from the point in the fundamental zone of Rodriguez space, 5 where all projection lines for pole figure inversion of the corresponding grain cross ͑each of the observed scattering vectors defines one of these projection lines in Rodriguez's space͒.…”
Section: Indexing From Friedel Pairsmentioning
confidence: 99%
“…(Hamilton, 1844;Tait, 1890;du Val, 1964;Altmann, 1966, Conway, Smith, 1992etc.). The application of quaternions to the description of reorientations of a cubic lattice and the associated equivalence classes of rotations was introduced by Grimmer (1974a) and extended to other lattice types by Grimmer (1980) and Heinz and Neumann (1991).…”
Section: Quaternion Methodsmentioning
confidence: 99%
“…This 'reduced' equivalence class may contain as many as 2g 2 rotations, where g is the order of the group of rotational symmetries of L. An important problem is the selection of a unique rotation as a definitive representative of its equivalence class. The convention usually adopted is to select the rotation with the smallest rotation angle q and with axis n corresponding to a point in a chosen fundamental region of the stereogram associated with the point symmetry group of L (Grimmer, 1980;Heinz, Neumann, 1991). Clarification of this latter concept is provided by Fig.…”
Section: Equivalence Classes Of Rotationsmentioning
confidence: 99%
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“…The lattice strain pole figures for a diffraction volume contain sufficient data to determine a strain orientation distribution function for that volume. Here, we define that distribution over the fundamental region of Rodrigues space using finite element (FE) interpolation [16] [25]. From the strain distribution, a crystal stress distribution is readily computed using Hooke's law.…”
Section: Introductionmentioning
confidence: 99%