Cmb. Henderson et al., AN EXAFS STUDY OF THE LOCAL STRUCTURAL ENVIRONMENTS OF FE, CO, ZN ANDMG IN NATURAL AND SYNTHETIC STAUROLITES, Mineralogical Magazine, 61(5), 1997, pp. 613-625
X-ray absorption spectroscopy (XAS) has been used to study the local s
tructures of Fe, Co, Zn, and Mg in synthetic and natural staurolites.
Results for the near-edge features (XANES) and refined EXAFS were used
to deduce the crystallographic site(s) occupied for each element. The
least squares refined, mean first shell metal-O bond lengths, coordin
ation numbers, and Debye-Waller factors are in the ranges: Fe 1.97-1.9
9 Angstrom, 3.5-4.1, 0.013-0.023 Angstrom(2); Co 1.97-1.98 Angstrom, 3
.5-3.9, 0.009-0.014 Angstrom(2); Zn 1.95-1.96 Angstrom, 3.7-3.8, 0.008
-0.009 Angstrom(2); and Mn 1.99 Angstrom, 3.8, 0.012 Angstrom(2). No s
ignificant differences were found which depended on element concentrat
ion or whether the sampes are synthetic or natural. The refined bond l
ength for Mg in end-member Mg-staurolite is 2.00 Angstrom but EXAFS da
ta did not allow refinement to give reliable coordination number and D
ebye-Waller factor estimates. The EXAFS data, together with staurolite
and model compound XANES features, suggest that > about 90% of Fe, Co
, Zn and Mn are concentrated in the tetrahedral T2 site, while in Mg-s
taurolite > about 75% of the total Mg is in T2 with the remainder in o
ctahedral sites. In natural staurolite from Pizzo Forno (PF2), a great
er proportion of Mg appears to be in octahedral coordination.