J. Appl. Cryst. (2002). 35, 455-458 [ doi:10.1107/S0021889802008038 ]
Abstract: A special kind of triangular dendrite of LiAlSiO4-SiO2 (or Li1-xAl1-xSi1+xO4, 0
x
1) in matt glaze has been observed by DIC (differential interference contrast) microscopy. This triangular dendrite is
-quartz with a sixfold-symmetric structure. For polyhedral crystals, a crystal with threefold-symmetric structure prefers to develop a hexagonal prismatic habit rather than a trigonal prismatic habit, because a trigonal prism has a higher surface energy than a hexagonal prism. However, for dendritic crystals, a special kind of triangular dendrite, with a pattern formed by the aggregation of many small triangles, can develop. As supercooling decreases,
-quartz can develop a series of morphologies with different surface energies, from snowflake-shaped dendrite to triangular dendrite, and finally to a polyhedral crystal in the form of a hexagonal prism. This series of crystal morphologies shows a morphological evolution from dendrite to polyhedral crystal, and also shows a morphological evolution between sixfold and threefold symmetries.
Keywords: minerals; crystal morphology; crystal habit;
-quartz; dendrite; differential interference contrast.
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