Crystal Structure of Coalingite

J. Pastor-Rodriguez and H. F. W. Taylor
Department of Chemistry, University of Aberdeen, Scotland

Summary: The crystal structure of coalingite (Mg10Fe2(OH)24(CO3)·2H2O) has been determined using single-crystal X-ray methods. The mineral is trigonal, with space group R3¯m, aH = 3·12, cH = 37·4 Å, Z = 12, and (0001) cleavage. The structure is of a layer type, and is based on a structural element about 12·5 Å thick in the c-direction and consisting of two brucite-like layers and one disordered layer containing carbonate ions and water molecules and resembling those in sjögrenite and pyroaurite. The unit cell comprises three of these structural elements stacked together in the c-direction. The Mg2+ and Fe3+ ions are randomly distributed among all the octahedral sites of the brucite-like layers. The structure closely resembles those of sjögrenite and pyroaurite, but has two brucite-like layers between each CO32−−H2O layer where these have one. There is a tendency to random interstratification, and the crystals appear to contain intergrown regions of brucite and of sjögrenite or pyroaurite. Coalingite-K probably has a similar structure, but with three brucite-like layers between each CO32−−H2O layer; its idealized formula is probably Mg16Fe2(OH)36(CO3).2H2O.

Mineralogical Magazine; September 1971 v. 38; no. 295; p. 286-294; DOI: 10.1180/minmag.1971.038.295.02
© 1971, The Mineralogical Society
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