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Certain complex, sulfur‐containing sodalite‐type silicates, synthesis of which is described, exhibit under 3650 Å excitation an emission extending from 5000 Å to beyond 7000 Å, the spectrum varying with composition. The band structure of this emission at −196°C is similar to the emission structure shown by a mixture of and . It is concluded that luminescence is due to the presence of , which replaces part of the normally present in sodalite. Synthetic sodalites containing both and are tenebrescent, coloring purple on irradiation with 2537 and 3650 Å ultraviolet.
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Russell D. Kirk (1954) studied this question.
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