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Large crystals of two siliceous zeolites have been grown and studied as a function of temperature using bifrefringence microscopy. In one case organic template is retained and the crystals show a reversible, ferroelastic phase transition on heating and cooling, but in another the bifrefringence indicates migration of organic template to the crystal edges upon heating.

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It is found that in LiTaO3 crystals with compositions between congruent and stoichiometric and in mixed LiNbxTa1-xO3 crystals self-organized stripes appear whose widths vary with temperature. They are broad and indistinct when the birefringence is close to zero and become narrower as the temperature is decreased or increased.

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The average structure of Na0.5Bi0.5TiO3 was found to possess non-rhombohedral symmetry, as supported by the splitting of Bragg peaks in the high-resolution reciprocal space maps.
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