Abstract
High-resolution solid-state 27Al nmr spectroscopic data indicate that the pentahedrally coordinated B site of vesuvianite is at least partially occupied by Al in Fe-poor, Mg-rich vesuvianites. The isotropic 27Al chemical shifts are 41.1 (±0.5) ppm for the 5-coordinated site and 9.0 and 2.5 (± 1) ppm for the octahedrally coordinated A and AlFe sites, respectively. These results were obtained using a recently developed technique based on observing the ±(3/2,1/2) satellite transitions of nuclides with spin I = 5/2, which provides a substantial increase in resolution relative to traditional massnmr examination of the central transition. The 29Si nmr spectra of the same samples contain a broad resonance at -80 ppm.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.