1968
DOI: 10.1139/p68-137
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ESR spectrum of Fe+3 in topaz. II. Superhyperfine structure

Abstract: The superhyperfine structure (shfs) aspect of the ESR spectrum of Fe+3 impurity in topaz (A12Si0,F2) has been investigated at X-band frequencies. The shfs tensors of the two inequivalent 19F nuclel have been determined. The experimental results were analyzed in the fornlalisnl of the effective spin. The isotropic contributions to shfs tensors were found to be (in cm-') 25.6 and 30.0 and the dipolar contribution, 6.8 and 5.9, with errors of k 0 . 5 (see Table V). The calculations leading to these values assume … Show more

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Cited by 7 publications
(4 citation statements)
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“…The valence states of Ti 3+ , Cr 3+ , Mn 3+ and Fe 3+ in imperial topaz were confirmed by EPR (Schott et al (2003). In agreement with the studies carried out by Thyer et al (1967), Holuj and Quick (1968) and Schott et al (2003), all based on EPR results, Fe 3+ substitutes for Al 3+ in the crystal structure of topaz. The replacement of Al 3+ by Ga 3+ was described by Northrup and Reeder (1994) and Breiter et al (2013).…”
Section: Discussionsupporting
confidence: 92%
“…The valence states of Ti 3+ , Cr 3+ , Mn 3+ and Fe 3+ in imperial topaz were confirmed by EPR (Schott et al (2003). In agreement with the studies carried out by Thyer et al (1967), Holuj and Quick (1968) and Schott et al (2003), all based on EPR results, Fe 3+ substitutes for Al 3+ in the crystal structure of topaz. The replacement of Al 3+ by Ga 3+ was described by Northrup and Reeder (1994) and Breiter et al (2013).…”
Section: Discussionsupporting
confidence: 92%
“…The presence of Fe 3+ impurity at A13+ sites in topaz has been reported (Thyer et al, 1967). All crystals of topaz are also known to have a concentration of F-up to about 20 % by weight (Thyer et al, 1967) and replacement of F-by OH-has been demonstrated by the OH absorption peak at 2.745 pm (Holuj & Quick, 1968). Substitution of OH-for F-has also been predicted by Rosenberg (1967) from X-ray and optical studies.…”
Section: (A) General Structurementioning
confidence: 97%
“…Since the F-content (20 % by weight) of topaz can be replaced by OH- (Rosenberg, 1967;Holuj & Quick, 1968) and the AI a+ content can be replaced by Fe a+, it is possible that the planar faults are thin layers of an exsolved phase involving OH-and/or Fe 3÷.…”
Section: (I) Planar Faultsmentioning
confidence: 99%
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