D. Nyfeler et al., NCHWANINGITE, MN22-CENTER-DOT-H2O, A NEW PYROXENE-RELATED CHAIN SILICATE FROM THE NCHWANING MINE, KALAHARI MANGANESE FIELD, SOUTH-AFRICA(SIO3(OH)(2)), The American mineralogist, 80(3-4), 1995, pp. 377-386
Nchwaningite, Mn22+SiO3(OH)(2) . H2O, is an orthorhombic chain silicat
e [space group Pca2(1), Z = 4, a = 12.672(9), b = 7.217(3), c = 5.341(
2) Angstrom], occurring as aggregates shaped like pin cushions, togeth
er with calcite, bultfonteinite, and chlorite at N'chwaning mine, loca
ted in the Kalahari manganese field, northern Cape Province, South Afr
ica. The aggregates consist of light brown, transparent needles, which
average 1.0 x 0.1 x 0.05 mm in size. Nchwaningite is named after the
mine N'chwaning II, where it was found first. Nchwaningite is biaxiall
y negative with the refractive indices alpha = 1.681(2), beta = 1.688(
2), gamma = 1.690(2), 2 V-x = 54.4(4)degrees. The optical orientation
is X = b, Y = a, Z = c. Nchwaningite has two perfect cleavages paralle
l to (010) and(100). The calculated density is 3.202 g/cm(3). The chem
ical composition, as determined by electron microprobe analyses, indic
ates minor substitutions of Mg for Mn. The crystal structure, includin
g H positions, was solved and refined from X-ray single-crystal data t
o R = 2.14%, R(w) = 2.91%. The nchwaningite structure consists of doub
le layers of laterally linked so-called truncated pyroxene-building un
its formed by a double chain of octahedra, topped with a Zweier single
chain of Si tetrahedra. Symmetry-equivalent units are linked laterall
y but turned upside down. This yields a double-layer structure with H
bridges linking the layers. A striking feature of the structure is tha
t one MnO6 corner is formed by a H2O molecule. The tetrahedral chain a
nd octahedral distortion of the new mineral is compared with pyroxenes
having Mn2+ in M1 [synthetic MnSiO3 (P2(1)/c clinopyroxene) and johan
nsenite CaMn(SiO3)(2)]. To test a complete Ca and Mg substitution for
Mn in the new nchwaningite structure type, distance least-square refin
ements were performed. It was found that Ca and Mg analogues would als
o yield reasonable interatomic distances and polyhedra.