Abstract
Cation order among the octahedral sites of three polycrystalline 29Si-enriched garnets on the enstatite-pyrope join has been examined using 29Si and 27Al MAS NMR spectroscopy. All three samples yielded 29Si NMR peaks in the chemical shift range of -68 to -90 ppm, caused by [4]Si, and a peak between -195.6 and -197.5 ppm, caused by [6]Si. The [4]Si/[6]Si ratios are consistent with the compositions. The changes in the 29Si chemical shifts for [4]Si with substitution of Mg for Si on the NNN octahedral sites are pairwise rather than directly additive. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 704-712 |
| Number of pages | 9 |
| Journal | American Mineralogist |
| Volume | 77 |
| Issue number | 7-8 |
| State | Published - 1992 |
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