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Electron Microprobe and Optical Absorption Study of Colored Kyanites
The characteristic blue color of the mineral kyanite is shown to be caused by traces of Ti$^{+++}$ in the range of a few parts per million. Evidence from the intensity and position of optical absorption bands indicates that the unusually intense color probably arises from electron delocalization int...
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Published in: | Science (American Association for the Advancement of Science) 1967-11, Vol.158 (3803), p.915-917 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The characteristic blue color of the mineral kyanite is shown to be caused by traces of Ti$^{+++}$ in the range of a few parts per million. Evidence from the intensity and position of optical absorption bands indicates that the unusually intense color probably arises from electron delocalization into narrow d-bands. |
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ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.158.3803.915 |