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Zeolites
McCusker, L.B. and Baerlocher, C., International Tables for Crystallography (2019). Vol. H, ch. 4.6, pp. 452-464 [ doi:10.1107/97809553602060000961 ]
with an ordering of framework atoms (e.g. the alternation of Al and P in an aluminophosphate). But it can also be quite complicated. For example, an aluminophosphate with the simple cubic sodalite framework type (SOD, 1 T atom) was synthesized using ...

X-ray diffraction methods: polycrystalline
Parrish, W., Wilson, A. J. C. and Langford, J. I., International Tables for Crystallography (2006). Vol. C, ch. 5.2, pp. 491-504 [ doi:10.1107/97809553602060000596 ]
as in (5.2.3.2) – arising from any specified aberration may increase as θ increases, but ordinarily this increase is insufficient to outweigh the effect of the factor. In the simple cubic case, one can write where K is a proportionality factor ...

Powder diffraction of superconductors
Huang, Q., International Tables for Crystallography (2019). Vol. H, ch. 7.13, pp. 868-884 [ doi:10.1107/97809553602060000987 ]
are the reflections corresponding to a cubic lattice, and the thin blue lines are the reflections due to the peak splitting or the superlattice peaks. (a) Reflections from a simple cubic lattice; (b), (c) and (d) reflections from tetragonal ...

Guide to the use of the scanning tables
Kopskyacute, V. and Litvin, D. B., International Tables for Crystallography (2010). Vol. E, ch. 5.2, pp. 395-420 [ doi:10.1107/97809553602060000788 ]
London Ser. A, 386, 95–143. Google Scholar Saint-Grégoire, P., Janovec, V. & Kopský, V. (1997). A sample analysis of domain walls in simple cubic phase of C 60 . Ferroelectrics, 191, 73–78. Google Scholar ...

Domain structures
Janovec, V. and Přívratská, International Tables for Crystallography (2013). Vol. D, ch. 3.4, pp. 484-559 [ doi:10.1107/97809553602060000918 ]


Representations of crystallographic groups
Janssen, T., International Tables for Crystallography (2013). Vol. D, ch. 1.2, pp. 34-71 [ doi:10.1107/97809553602060000901 ]
For a simple cubic space group, the point [ ] is denoted by X . Its is the tetragonal group . All points [ ] with and form one stratum with point group . This stratum is denoted by etc . The strata can be compared with the Wyckoff ...

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