Crystal chemistry of the axinite-group minerals: A multi-analytical approach

Sixty axinite samples from 24 localities worldwide were characterized by el ectron microprobe analysis (EMPA) to define the limits of compositional var iation. Three samples are very close to the Mn, Fe, and Mg end-members. Ter nary (Mn,Fe2+,Mg)-compositions occur mostly in the ferroaxinite and mangana xinite fields, and are constrained by the relation Mg less than or equal to Fe. Core-rim chemical zoning was observed in 20 samples, with systematic e nrichment of Fe in the core and Mn in the rim, independent of sample proven ance. The chemical composition (including B, H, and Fe2+/Fe3+) of 17 homogeneous samples was investigated using electron-microprobe analysis, thermo-gravime try (TG), ion microprobe (SIMS), crystal-structure refinement (SREF), and M ossbauer spectroscopy (MS). For all samples except pure manganaxinite, most of the iron is Fe2+. The content of Fe3+ and the Fe3+/Sigma Fe ratio incre ase with Mn content up to 0.31 atoms per formula unit (apfu) and 0.80, resp ectively. Fe3+ may substitute for Al or also for divalent cations balanced by the OH deficiency: Fe3+ + O2- <----> Fe2+ + OH-, or Fe3+O(Fe2+OH)(-1) Boron content ranges from 1.88 to 2.07 apfu (+/-2.5% relative) and shows an inverse relation with Si content. Direct measurement of the B-tetrahedron size provides structural confirmation of the Si <----> B exchange. Hydroxyl deficiency accompanies this substitution and the following coupled mechani sm is proposed: Si4+ + O2- <----> B3+ + OH-, or SiO(BOH)(-1) Hydrogen content ranges from 1.7 to 2.1 apfu (+/-5% relative). The deficien cy of OH from the stoichiometric value of 2.0 per formula unit is related d irectly to the number of trivalent and tetravalent cations, as OH content p lays a crucial role in charge-balance relations. A revised chemical formula for the axinite-group minerals is proposed: ([6])[Ca(Ca1-xMnx)(Mn,Fe2+,Mg,Zn,Al-u,Fe-v(3+))(Sigma) (=) (1)(Al2-yFey3+)] (2)([4]) [(B1-zSiz)(2)Si-8]O-30(OH1-wOw)(2), where x less than or equal to 1, u < 1, v < 1, y < 1, z much less than 1, a nd w - (u + v + z).