eMagRes 1996
DOI: 10.1002/9780470034590.emrstm0188
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Geological Applications

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Cited by 1 publication
(3 citation statements)
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“…The composition of the materials could be estimated from the relative spectral intensities, which would be difficult to obtain with comparable precision from diffraction. The paramagnetic shifts observed were much smaller than those seen previously in 119 respectively, suggesting there is very little A/B mixing in these systems). This was also confirmed using DFT calculations, which predicted significantly different shifts for Y VI the cation lattice and of the anions/vacancies (i.e., both compositional and positional disorder).…”
Section: Ceramics and Oxidescontrasting
confidence: 59%
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“…The composition of the materials could be estimated from the relative spectral intensities, which would be difficult to obtain with comparable precision from diffraction. The paramagnetic shifts observed were much smaller than those seen previously in 119 respectively, suggesting there is very little A/B mixing in these systems). This was also confirmed using DFT calculations, which predicted significantly different shifts for Y VI the cation lattice and of the anions/vacancies (i.e., both compositional and positional disorder).…”
Section: Ceramics and Oxidescontrasting
confidence: 59%
“…However, the more covalent character of the Sn-O bond was shown to result in a greater through-bond (or Fermi contact) contribution to the paramagnetic interaction [96,97]. More recently, NNN substitution in diamagnetic Y Ti 2-x Sn x O 7 pyrochlores was studied using a combination of 89 Y and119 Sn NMR spectroscopy and DFT calculations [51,[82][83][84]119 Sn spectra inFigure 11ashow only Y VIII and Sn VI are present (i.e., Y and Sn sitting on the A and B sites of the pyrochlore structure,…”
mentioning
confidence: 99%
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