Ferrotitanowodginite, Fe2+TiTa2O8, a new mineral of the wodginite group from the San Elias pegmatite, San Luis, Argentina

Ferrotitanowodginite is a new mineral of the wodginite group, which is found in acid defined from two closely adjacent pegmatites in the San Luis province, Argentina, but previously encountered in the Tanco (Manitoba) and Marko's (Ontario) pegmatires. In the San Elias pegmatite, ferrotitanowodginite occurs aggregated with ferrowodginite and associated with microlite, ferrotapiolite, cleavelandite, and quartz. In La Viquita pegmatite, ferrotitanowodginite occurs in a replacement unit associated with wodginite, ferrowodginite, titanowodginite and ferrotapiolite in yellow muscovite and quartz. Ferrotitanowodginite is very dark brown to black, with a dark brown streak and submetallic luster. Mohs hardness is 5 1/2 and D-calc = 7.368 g/cm(3). In reflected light, it is creamy white and gray in air and oil, respectively; anisotropy is distinct, bireflectance and pleochroism moderate. Ferrotitanowodginite is monoclinic, space group C2/c, Z = 4. Unit-cell dimensions for San Elias' material are a = 9.403(4) Angstrom, b = 11.384(3) Angstrom, c = 5.075(1) Angstrom, beta = 90.550 (2), V = 543.24(22) Angstrom(3). The strongest lines in the X-ray powder diffraction are d = 2.953 Angstrom, I = 100%, (hkl = 22 (1) over bar); d = 2.939 Angstrom, I = 90% (hkl = 221); d = 3.626 Angstrom, I = 70% (hkl = 220); and d = 1.715 Angstrom, I = 50% (hkl = 402). Eighteen analyses by electron microprobe gave the following mean composition: WO3 0.02, Nb2O5 6.52, Ta2O5 70.68, TiO2 7.10, SnO2 1.25, ThO2 0.01, UO2 0.02, As2O3 0.03, Sb2O3 0.02, Bi2O3 0.03, Fe2O3 2.18, MgO 0.01, CaO 0.01, MnO 1.05, FeO 10.27, PbO 0.05, total 99.25 wt%. The La Viquita sample is much richer in Mn and Sn. The simplified formula for ferrotitanowodginite is: (Fe2+, Mn2+) (Ti,Sn4+,Ta,Fe3+) (Ta,Nb)(2)O-8, ideally Fe2+TiTa2O8.