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Figure 3
A diagram of the [Hg3O] pyramids in (a) eglestonite (Mereiter et al., 1992BB10) and (b) Hg3AlF6O2H. Hg atoms are dark grey, O atoms are white and H atoms are light grey. The inversion centre is denoted by a small black point. The broken bonds in (a) correspond to the connection to neighbouring Hg atoms of the Hg22+ dumb-bell.

Journal logoSTRUCTURAL
CHEMISTRY
ISSN: 2053-2296
Volume 58| Part 3| February 2002| Pages i37-i39
doi:10.1107/S0108270102000690
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