Woodallite, a new chromium analogue of iowaite from the Mount Keith nickeldeposit, Western Australia

Woodallite is a new Cr-rich member of the hydrotalcite group from the large , low-grade Mount Keith nickel deposit, in the northeastern Goldfields dist rict of Western Australia. Woodallite occurs as whorls and clusters of minu te platelets up to 6 mm across in lizardite+brucite-altered dunite. Individ ual platelets are typically 10-100 mum in maximum dimension and are often c urved. Associated minerals include chromite, lizardite, iowaite, pentlandit e, magnetite, tochilinite and brucite. Electron microprobe analysis gave: M g 25.90 wt.%; Cr 10.81; Fe 4.86; Al 0.68; Cl 9.89; S 0.03; Si 0.01; Ni 0.01 ; Na 0.01, yielding (after correction for loss of volatiles) an empirical f ormula of Mg-6.19(Cr1.21Fe0.51Al0.15)(Sigma1.87) (OH)(16)[Cl-1.62(CO3)(0.17 )(SO4)(0.01)]. 4H(2)O, by analogy with the hydrotalcite group. The simplifi ed formula is Mg6Cr2(OH)(16)Cl-2. 4H(2)O. Combined thermogravimetric analys is and mass spectroscopy showed a two-stage weight loss of 12.7% and 27.3% occurring over the ranges 25-300 degreesC and 300-660 degreesC, respectivel y. The first weight loss is attributed to loss of interlayer water, chlorin e-bearing species (e.g. HCl) and some CO2, the second to loss of hydroxide water, remaining CO2 and Cl species. The mineral is deep magenta to purple in colour, transparent, with a resinous to waxy lustre, and a perfect basal {0001} cleavage. Woodallite has a Mohs hardness of 1.5-2, and a pale-pink to white streak. The strongest lines in the X-ray powder pattern are [d(obs ) (I-obs) (hkl)] 8.037 (100) (003); 4.021 (48) (006); 2.679 (1) (009); 2.62 4 (3) (012); 2.349 (5) (015); 2.007 (6) (0,0,12); 1.698 (2) (0,1,11); 1.524 (2) (2 (1) over bar3). These lines were indexed on a hexagonal cell with a = 3.103(2), c = 24.111(24) Angstrom, V = 201.14 Angstrom (3) and Z = 3/8. The new mineral is isostructural with the hydrotalcite group and has space group R (3) over barm. The measured density is 2.062 gm/cm(3). Woodallite i s uniaxial negative with omega = 1.555 and epsilon = 1.535 (white light); p leochroism is distinct from violet to pinkish lilac. Woodallite forms as a result of hydrothermal alteration of primary magmatic chromite by Cl-rich s olutions at temperatures < 320 degreesC. Relict chromite fragments are freq uently present in the whorls, and associated magnetite is altered extensive ly to iowaite. The mineral is named after Roy Woodall, eminent Australian i ndustry geologist.