Abstract
The dichroism of tourmaline arises partially from charge-transfer transitions within nextnearest neighbour cations through shared octahedral edges in the 001 layer. Similar structural features occur in the sheet silicates, and charge-transfer spectra in these structures are discussed. © 1970.
Cite
CITATION STYLE
APA
Townsend, M. G. (1970). On the dichroism of tourmaline. Journal of Physics and Chemistry of Solids, 31(11), 2481–2488. https://doi.org/10.1016/0022-3697(70)90065-X
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