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Figure 1
(a) Rare-earth sites ([r \,\lt\, 40] Å around the origin) in the f-Zn–Mg–R icosahedral quasicrystals generated using the parameters determined by the synchrotron-radiation powder X-ray experiment (Ishimasa et al., 2003BB34). (b) Magnified illustration of the edge-sharing dodecahedral network of the rare-earth sites; only atoms participating in the network are shown.

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