Y. Kawachi et al., NOELBENSONITE, A NEW BAMN SILICATE OF THE LAWSONITE STRUCTURE TYPE, FROM WOODS MINE, NEW-SOUTH-WALES, AUSTRALIA, Mineralogical Magazine, 60(399), 1996, pp. 369-374
Noelbensonite, a new mineral, is the barium manganese analogue of laws
onite. It is described from the Woods ornamental rhodonite mine, 30 km
NNE of Tamworth, New South Wales, Australia, where it occurs as aggre
gates of blocky to sometimes lamellar crystals ranging from a few micr
ometres to (rarely) 100 mu m in length. It replaces NaMn amphibole, na
mansilite, and pectolite, and also occurs as tiny monomineralic veinle
ts 0.05-0.25 mm thick. Rare euhedral crystals are dominated by {100} a
nd {011}, with {011} (01(1) over bar) = 68 degrees. The mineral is ort
horhombic, space group apparently Cmcm; a = 6.325(1), b = 9.120(1), c
= 13.618(1) Angstrom, V = 785.6(1) Angstrom(3), with a : b : c = 0.694
: 1 : 1.493. Noelbensonite is brittle, fracture irregular, Mohs hardn
ess about 4, cleavage and twinning not observed, colour dark brown, st
reak paler yellow-brown, lustre earthy on some veinlet surfaces to bri
lliantly vitreous, calculated density 3.87 g/cm(3), refractive indices
alpha = 1.82(1), beta (calculated from 2V) = 1.835(10), gamma = 1.85(
1), biaxial negative 2V(alpha) = 46 degrees(3 degrees), strong dispers
ion r > nu, straight extinction to plane of flattening, {100}, alpha p
arallel to c, beta parallel to b, gamma parallel to a with pleochroism
in very thin sections: alpha = orange yellow, beta = orange, gamma =
brownish orange, absorption gamma > beta > alpha. The average of 23 el
ectron microprobe analyses (wt.%) is SiO2 26.02, Al2O3 0.17, TiO2 0.01
, Fe2O3 0.19, Mn2O3 34.76, CaO 0.31, Na2O 0.14, BaO 29.08, SrO 1.51, H
2Ocalc 7.87, total 100.06, leading to the simplified formula BaMn23+[S
i2O7](OH)(2) . H2O. Up to 15% Sr and 9% Ca substitute for Ba in the la
rge-cation sites. The strongest lines in the X-ray powder diffraction
pattern are [(I-obs) d(obs)/Angstrom hkl] (100) 4.85 111; (50) 4.557 0
20; (59) 4.322 021; (77) 3.416 113,004; (80) 2.869 202; (47) 2.849 114
; (82) 2.729 024; (45) 2.543 132; (48) 2.428 222; (38) 2.255 223,041.
The name is for William Noel Benson (1885-1957), in honour of his clas
sic researches in the New England Fold Belt and of his tenure of the C
hair of Geology at the University of Otago.