The 2 M 1 dioctahedral mica polytype: A crystal chemical study
The structure of dioctahedral true micas such as muscovite and celadonitic muscovite (2 M 1 polytype, space group C 2/ c ) is mostly affected by variations of the octahedral Al ( VI Al) content. Crystals with greater Mg, Fe substitutions ( i.e. celadonitic muscovite) reduce the dimensional differenc...
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Veröffentlicht in: | Clays and clay minerals 2005-04, Vol.53 (2), p.190-197 |
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Sprache: | eng |
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Zusammenfassung: | The structure of dioctahedral true micas such as muscovite and celadonitic muscovite (2
M
1
polytype, space group
C
2/
c
) is mostly affected by variations of the octahedral Al (
VI
Al) content. Crystals with greater Mg, Fe substitutions (
i.e.
celadonitic muscovite) reduce the dimensional difference between the larger
trans
-oriented
M
1 site and smaller
cis
-oriented
M
2 octahedral site. The octahedral anionic position
O
4 is displaced from the center of the hexagon, defined by 031 and 032 oxygen atoms (
i.e.
‘octahedral hexagon’), both on and off the (001) plane. The distance between interlayer cation
A
and
O
4 is smaller in more substituted species, thus providing different orientations of the
O
4−
H
vector, as a function of
VI
Al. Octahedral distances
( and
are expressed as a function of cell parameters and
VI
A1 content, thus allowing an approximate estimate of site dimensions. These approximations are useful when a detailed structural refinement is not available. In celadonitic muscovite, the octahedral hexagon mean edge (
Hex
) is not significantly affected by
VI
A1 content. The
VI
A1 increase produces both a decrease in cell lateral dimensions and a distorted ‘octahedral hexagon’. The decrease in
a
and
b
is consistent with a decrease of
Hex
, whereas the distortion of the’ octahedral hexagon’ is consistent with an increase of (
Hex
), because an irregular hexagon produces a longer mean edge than a regular hexagon of equal area.
The tetrahedral mean basal edge (
VI
<
O−O>
b
assal
) is reduced as celadonitic substitution progresses. The tetrahedral rotation angle, α was thus found to increase from celadonite to muscovite. However, in muscovite with
VI
Al content between 1.8 and 2.0 atoms per formula unit (a.p.f.u.), α approaches a saturation value, thus showing a proportional increase of tetrahedral and octahedral sheet lateral dimensions. Furthermore, α variation allows a coarse approximation of the threshold
VI
Al content, below which celadonitic substitution may not progress. |
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ISSN: | 0009-8604 1552-8367 |
DOI: | 10.1346/CCMN.2005.0530209 |