Clays and Clay Minerals, Vol. 58, No. 1, 62–71, 2010.
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Authors
Kogure, Toshihiro
Elzea-kogel, Jessica
Johnston, Cliff T.
Bish, David L.
Issue Date
2010
Type
Article
Language
Keywords
Periodicals , Geology , FTIR , HRTEM , Kaolinite , SAED , Stacking Fault
Alternative Title
Stacking Disorder In A Sedimentary Kaolinite
Abstract
Although structural disorder in kaolinite has been investigated extensively, it is still not understood properly. To investigate the problem, a kaolinite specimen of sedimentary origin from Capim, Brazil, was examined, mainly by transmission electron microscopy (TEM). Selected-area electron diffraction (SAED) along the Xi ([100], [110], and [11¯0]) directions shows various features, from completely discrete patterns to heavily streaked ones along the c* direction, suggesting that the degree of stacking disorder is variable among individual grains. High-resolution TEM images indicate that stacking faults are mainly caused by disorder of alternating t1 (~-a/3) and t2 (-a/3 +b/3) layer displacements. Furthermore, stacking faults have been observed (1) as isolated stacking faults (e.g. insertion of an isolated t2 ‘fault’ in an ordered sequence with t1 layer displacement) and (2) as interstratification of two kinds of multilayer blocks having regular t1 and t2 layer displacements. A mixture of grains with various degrees and modes of disorder with alternating t1 and t2 layer displacements may explain the experimental profile of the 02, 11 X-ray diffraction band. Faults related to displacement of the octahedral vacancy and/or to layer rotation were also observed in HRTEM images. The SAED patterns along the Yi ([010], [310], and [31¯ 0]) directions occasionally have extra spots and/or streaks, suggesting the presence of stacking sequences with (K60º, 180º) mutual layer rotation and/or with (0, Kb/3) layer displacements. The local dickite or nacrite-like fragments formed by these faults are in qualitative agreement with recent low-temperature FTIR results from this sample, where distinct n(OH) absorption bands reflect multiple interlayer O-H_O environments that are possibly ascribed to dickite and nacrite.
Description
gsccm58106-kog.pdf : 1,027KB
Citation
Clays and Clay Minerals, Vol. 58, No. 1, 62–71, 2010.
Publisher
The Clay Minerals Society
License
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