Abstract
Summary
The structural formula of stilpnomelane
averaged from 37 representative literature
analyses and based on the determined structure is
(Ca,Na,K)4(Ti0·1Al2·3Fe35·5Mn0·8Mg9·3)[Si63Al9](O,OH)216·nH2O.
Ferrostilpnomelanes have up to 12
R3+
cations in the octahedral sheet,
ferristilpnomelanes commonly have between 24 and
30
R3+
cations, rarely up to 37. The two groups can be
distinguished by accurate X-ray powder
diffraction, ferrostilpnomelanes having
d001
less and a greater than
have ferristilpnomelanes. The unit cell is
triclinic, a =
b∼21·8 Å,
γ = 120°,
d001∼12·2
Å,
P.
Hexagonal groups or ‘islands’ of 24 silicon-oxygen
tetrahedra co-ordinate to the octahedral sheet,
the centres of the ‘islands’ are displaced by
5a/12,
8b/12 on either side of
the octahedral sheet as a result of warping of
this sheet to permit articulation with the smaller
tetrahedral sheet. The 24-tetrahedra ‘islands’ are
linked laterally by 6-member rings of inverted
tetrahedra, which in turn link at their apices to
like rings connecting the next sheet of ‘islands’.
Thus a single tetrahedral layer is 4 tetrahedra
thick and has symmetry
6/m. The 6-member rings
of tetrahedra act as hinges permitting up to 0·5 Å
extension or contraction of the tetrahedral sheet
to accommodate variations in the octahedral sheet
dimensions with varying
R2+/R3+
ratio.
Subject
Geochemistry and Petrology
Cited by
51 articles.
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