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Crystal structure study of a cobaltoan dolomite from Kolwezi, Democratic Republic of Congo

A structural study has been undertaken on a cobaltoan dolomite, with chemical formula CaMg(0.83)Co(0.17)(CO(3))(2) (cal­cium magnesium cobalt dicarbonate), from Kolwezi, Democratic Republic of Congo. Pale-pink euhedral cobaltoan dolomite was associated with kolwezite [(Cu(1.33)Co(0.67))(CO(3))(OH)(2...

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Detalles Bibliográficos
Autor principal: Perchiazzi, Natale
Formato: Online Artículo Texto
Lenguaje:English
Publicado: International Union of Crystallography 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4350686/
https://www.ncbi.nlm.nih.gov/pubmed/25844202
http://dx.doi.org/10.1107/S2056989015003126
Descripción
Sumario:A structural study has been undertaken on a cobaltoan dolomite, with chemical formula CaMg(0.83)Co(0.17)(CO(3))(2) (cal­cium magnesium cobalt dicarbonate), from Kolwezi, Democratic Republic of Congo. Pale-pink euhedral cobaltoan dolomite was associated with kolwezite [(Cu(1.33)Co(0.67))(CO(3))(OH)(2)] and cobaltoan malachite [(Cu,Co)(2)(CO(3))(OH)(2)]. A crystal with a Co:Mg ratio of 1:5.6 (SEM/EDAX measurement), twinned on (11 -2 0) was used for crystal structural refinement. The refinement of the structural model of Reeder & Wenk [Am. Mineral. (1983 ▸), 68, 769–776; Ca at site 3a with site symmetry -3; Mg site at site 3b with site symmetry -3; C at site 6c with site symmetry 3; O at site 18f with site symmetry 1] showed that Co is totally incorporated in the Mg site, with refined occupancy Mg(0.83)Co(0.17), which compares with Mg(0.85)Co(0.15) from chemical data. The Co substitution reflects in the expansion of the cell volume, with a pronounced increasing of the c cell parameter.