Journal
EUROPEAN JOURNAL OF MINERALOGY
Volume 28, Issue 3, Pages 593-599Publisher
E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG
DOI: 10.1127/ejm/2016/0028-2542
Keywords
tourmaline; gallium; synthesis; crystal structure; Mossbauer spectroscopy; X-ray single-crystal analysis
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Crystals of Ga-rich, Fe-bearing tourmaline (similar to 25 wt% Ga2O3, 11 wt% FeOtotal) were grown from hydrothermal solution at 100 MPa and 600 degrees C. The crystals were grown on a seed as a newly formed, up to 200 gm thick layer and, in addition, as free, spontaneously nucleated elongated prisms, 10 to 200 gm in size. The crystal structure of the synthetic tourmaline was studied by Mossbauer spectroscopy and single-crystal X-ray diffraction (to an R-index of 0.032; a= 16.000(1), c = 7.257(1) angstrom). Gallium and iron cations are distributed over the Y and Z octahedral sites according to the crystal-chemical formula (Na-0.95 square(0.05)) (Ga1.34Fe0.622+Al0.44Fe0.343+Ni0.26) (Al3.28Ga1.92Fe0.412+Fe0.393+) (Si6O18) (BO3)(3) (OH2.29O0.71) (O), suggesting that the disordered distribution previously shown for Al3+ also holds for other trivalent cations in tourmalines.
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