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Other crystalline rocks, the metamorphic rocks such as marbles, mica-schists and quartzites, are recrystallized.
This means that they were at first fragmental rocks like limestone, shale and sandstone and have never been in a molten condition nor entirely in solution, but the high temperature and pressure conditions of metamorphism have acted on them by erasing their original structures and inducing recrystallization in the solid state Specific industrial techniques to produce large single crystals (called boules) include the Czochralski process and the Bridgman technique.
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The scientific study of crystals and crystal formation is known as crystallography.The International Union of Crystallography has redefined the term "crystal" to include both ordinary periodic crystals and quasicrystals ("any solid having an essentially discrete diffraction diagram"). Conversely, these properties are not quite exclusive to crystals.They can appear in glasses or polycrystals that have been made anisotropic by working or stress—for example, stress-induced birefringence.They have many attributes in common with ordinary crystals, such as displaying a discrete pattern in x-ray diffraction, and the ability to form shapes with smooth, flat faces.Quasicrystals are most famous for their ability to show five-fold symmetry, which is impossible for an ordinary periodic crystal (see crystallographic restriction theorem).
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These have no periodic order, even microscopically.