Abstract
The ESR spectra of several turquoise specimens contained an anisotropic component which was due to Cu2+ and an isotropic component arising from Fe3+ ions. The Fe/Cu concentration ratio obtained from these measurements agreed with ratios obtained analytically. A variable-temperature study from 77 K to 560 K indicated that the cupric ions are paramagnetic while the ferric ions behave antiferromagnetically at low temperatures.
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