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Natural graphite single crystals and polycrystals have been deformed at room temperature and optical and electron microscope studies of these have been coupled with x-ray investigations. The appearance and disappearance of x-ray diffraction peaks corresponding to the rhombohedral structure has been investigated. After plastic shearing the graphite crystals contain many tilt and twist boundaries and are profusely twinned. A mechanism is proposed for the production of the rhombohedral form.
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Freise et al. (1963) studied this question.
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