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- W2092355768 abstract "Model fabric patterns for translation gliding in rock salt are constructed on the basis of two metallurgical theories for intragranular slip. For statistically homogeneous types of pure mesoscopic distortion, Calnan and Clews theory predicts the intragranular rotations leading to patterns of preferred orientation of 〈100〉. Dillamore and Roberts' theory, on the other hand, permits rotational fluctuations of the principal axes, which makes the models more realistic. Eleven different model patterns, referred to principal axes of deviatoric mesoscopic stress, are obtained for different types of distortion, but five models are considered to be most applicable to domal salt. The various model patterns are subsequently compared with natural halite fabrics for 13 domains of fairly homogeneous strain in two Gulf Coast Domes. These domains (specimens) were taken from macroscopic folds, whose axes and axial “planes” serve as common reference elements for natural fabrics and models. It is assumed that the directions of greatest finite extension and compression are subparallel to fold axes and axial plane normals, respectively. In some fabric diagrams for domal salt, 〈100〉 -poles outline maxima, and distinct but generally incomplete girdles. Other diagrams show a trend toward random orientation of 〈100〉. Most of the former diagrams exhibit fabric patterns that resemble those of the five realistic models after Dillamore and Roberts. This suggests translation gliding to be the dominant mechanism of tectonic flow, which may be succeeded by annealing recrystallisation, whereby the deformational patterns are increasingly blurred and finally destroyed." @default.
- W2092355768 created "2016-06-24" @default.
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- W2092355768 date "1968-04-01" @default.
- W2092355768 modified "2023-09-26" @default.
- W2092355768 title "Intragranular gliding in domal salt" @default.
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- W2092355768 doi "https://doi.org/10.1016/0040-1951(68)90001-2" @default.
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