1997
DOI: 10.1107/s0108767396013438
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Moiré Fringes and/or Translation-Fault Fringes?

Abstract: Interference fringes on transmission topographs of crystals with an implanted amorphous layer are, among others, attributed to the moir6 or the translation-fault effect. This discussion is reconsidered in the frame of the theory of a perfect bicrystal extended to a deformed one. It is shown that translation-fault fringes have the same properties as moir6 fringes and that it is not necessary to introduce translation-fault fringes as a new diffraction phenomenon.

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Cited by 39 publications
(10 citation statements)
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“…The origin of the observed fringe systems is still unclear although the possibilities seem to be limited to (a) Moire´fringes due to the superposition in the direction of the diffracted beam of different crystal volumes having slightly different misalignment or lattice parameters [27] or (b) Pendello¨sung fringes due to the presence of wedge-shaped crystal volumes [28].…”
Section: Discussionmentioning
confidence: 99%
“…The origin of the observed fringe systems is still unclear although the possibilities seem to be limited to (a) Moire´fringes due to the superposition in the direction of the diffracted beam of different crystal volumes having slightly different misalignment or lattice parameters [27] or (b) Pendello¨sung fringes due to the presence of wedge-shaped crystal volumes [28].…”
Section: Discussionmentioning
confidence: 99%
“…Simon & Authier (1968), and Gerward (1973) reported moiré fringes observed in ion-implanted silicon crystals. Although referred to their observed fringes as 'translation fault' fringes , Ohler et al (1997) later explained that they are essentially moiré fringes. Moiré fringes observed with a monolithic type bicrystal, prepared by making a saw cut in a single crystal, were reported by Hashizume et al (1972) and Tanemura & Lang (1973).…”
Section: Introductionmentioning
confidence: 99%
“…Consequently, the misaligned growth sectors could produce some degree of stress inside the crystal lattice and wedge-shaped volumes. Therefore, the origin of the observed fringes is considered to be due to Moire fringes due to the superposition in the direction of the diffracted beam of different crystal volumes having slightly different misalignment or lattice parameters 37 or Pendellösung fringes due to the presence of wedge-shaped crystal volumes. 38 For the orthorhombic form, as shown in Figure 3, not only dislocation lines but also growth sector boundaries (marked OSB) were clearly observed.…”
Section: Resultsmentioning
confidence: 99%