Quartz Crystals and Their Colors
- 1 April 1973
- journal article
- review article
- Published by Wiley in Angewandte Chemie International Edition in English
- Vol. 12 (4) , 283-291
- https://doi.org/10.1002/anie.197302831
Abstract
The many colors found in quartz crystals are always due to the presence of impurity atoms, whose concentrations rarely exceed 0.1 wt.%. The impurity atoms occupy either silicon sites in the lattice or interstitial sites in the channels parallel to the c axis of the quartz structure; very fine precipitations of foreign phases are sometimes also observed, though this is less common. In addition to intrinsic colors of transition metal ions, one also finds color centers produced by ionizing radiation. Regular distributions of impurity atoms and colors may develop in the crystals as a result of some factor connected with its growth. Most of the natural quartz colors, as well as others that do not occur in nature, have been produced in synthetic quartzes.Keywords
This publication has 41 references indexed in Scilit:
- The structure of yellow iron centres in quartzPhysica Status Solidi (b), 1971
- Paramagnetic Resonance Centres in Amethyst and Citrine QuartzNature, 1966
- Optical and Paramagnetic Properties of Iron Centers in QuartzThe Journal of Chemical Physics, 1966
- Titanium Colour Centres in Rose QuartzNature, 1963
- Paramagnetic Resonance of Color Centers in Germanium-Doped QuartzThe Journal of Chemical Physics, 1959
- Paramagnetic Resonance Spectrum of Manganese in Single Crystals of Alkali Halides Grown from SolutionsProceedings of the Physical Society. Section B, 1956
- Paramagnetic Resonance of Manganese in Single Crystals of Alkali HalidesProceedings of the Physical Society. Section B, 1956
- Paramagnetic Resonance in Neutron-Irradiated Diamond and Smoky QuartzNature, 1954
- Optical Absorption and Photoconduction in the Visible and Near Infrared in Single Crystals of BaOPhysical Review B, 1953
- Die Verfärbung von MgO-Kristallen durch gittereigene BausteineThe European Physical Journal A, 1951