Abstract
Pyrope-grossular solid solutions, (Mg,Ca)3Al2Si3O12, of composition Py85Gr15 and Py75Gr25 were synthesized at 1000, 1200, and 1400 °C and 30 kbars in a piston-cylinder device. The synthetic garnets were characterized using optical, microprobe, and X-ray methods and their Ca-Mg distributions were investigated using 29Si MAS NMR spectroscopy. The syntheses produced 100% garnet except for those undertaken at 1000 °C, where small amounts (up to 3%) of clinopyroxene were present. X-ray powder refinements showed differences up to 0.01 Å in the unit-cell dimension of the garnets synthesized at the three different temperatures. A general decrease of the X-ray diffraction line widths with increasing synthesis temperature is observed. The 29Si NMR spectra of Py85Gr15 show little change as a function of synthesis temperature. In the spectra of Py75Gr25 small but measurable changes in the relative peak intensities, depending upon synthesis temperature, were observed with a more random cation distribution corresponding to a higher synthesis temperature. None of the garnets investigated has a completely random Ca-Mg distribution. The reduction in configurational entropy compared to the disordered state is estimated to be less than 2 J/mol·K.
| Original language | English |
|---|---|
| Pages (from-to) | 1422-1432 |
| Number of pages | 11 |
| Journal | American Mineralogist |
| Volume | 84 |
| Issue number | 9 |
| DOIs | |
| State | Published - Sep 1999 |
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