M. Kochmuller et al., CRYSTAL-STRUCTURE REFINEMENT OF SYNTHETIC FE-STAUROLITE AND MG-STAUROLITE BY RIETVELD ANALYSIS OF X-RAY POWDER-DIFFRACTION DATA, European journal of mineralogy, 10(3), 1998, pp. 453-460
The crystal structure of Fe-staurolite, synthesized at 5 and 25 kbar a
nd 680 degrees C, and of Mg-staurolite, synthesized at 25 kbar and 700
degrees C, has been refined from X-ray powder-diffraction data using
the Rietveld method in the space group Ccmm. The study was aimed to ge
t insight into the distribution of Fe2+, Mg and Al at the tetrahedral
T2 and the octahedral M4 sites. Fe-staurolite synthesized at 25 kbar d
iffers from that at 5 kbar by a lower Fe2+ content (2.84 instead of 3.
12 pfu) and higher Al content (0.60 instead of 0.32 pfu) at T2. Mg-sta
urolite synthesized at 25 kbar differs from the 25-kbar Fe-staurolite
by higher occupancy of Mg at M4 (0.88 pfu), compared with 0.20 Fe2+ pf
u in the case of Fe-staurolite, accompanied with less Mg at T2 (2.12 p
fu) and only a small amount of Al at T2 (0.16 pfu).