Mineralogical Journal
Online ISSN : 1881-4174
Print ISSN : 0544-2540
ISSN-L : 0544-2540
NEW UNIT LAYERS FOR MICAS
HIROSHI TAKEDARYOICHI SADANAGA
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1969 Volume 5 Issue 6 Pages 434-449

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Abstract
A new choice of unit layer proposed by Sadanaga & Takeda (1968) has been found useful for explaining the two characteristic features of the X-ray diffraction pattern of the mica, namely, the periodic intensity distribution and the partial enhancement of symmetry. The recognition of the fact that the symmetry of the new unit layers is higher than that of the crystal, played an important role in the derivation of intensity distribution functions.
By the introduction of four kinds of layer with either trigonal or hexagonal symmetry and designated D, D*, T and T*, the layer sequence of any mica polytype can be described by stacking of these layers in parallel orientation and with mutual staggers of 1/3·a1, 1/3·a2 and 1/3·a3. With the aid of these new unit layers, it is proposed a new symbol to describe the stacking sequence of mica, together with a convention of axial settings to specify the symbol uniquely.
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© Japan Association of Mineralogical Sciences
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