Ceramics-Silikáty 26, (1) 7 - 13 (1982) |
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THE ROLE OF Ti⁴+ IN THE CRYSTAL STRUCTURE OF PYROXENE ISOMORPHOUS SERIES: DIOPSIDE (CaMgSi₂O₆)—CaTiAl₂O₆ |
Fejdi Pavel |
Department of Mineralogy and Crystallography, Natural Science Faculty of the Comenius University, Gottwaldovo nám. 19, 886 02 Bratislava
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The crystal structure of a model-system clinopyroxene of approximate 72 mole % diopside-28 mole % CaTiAl₂O₆ solid solution was refined. The space group is C2/c, cell parameters a = 9.781(5), b 8.856(4), c = 5.331(3) 10-10 m, β = 106.06 (5)°. The problem of Ti4+ location was solved by the least-squares refinement and difference Fourier syntheses to an R-value 6.1 %. The Ti4+ presumably occupy the M1 site but a small part of Ti4+ is placed in the tetrahedraly coordinated positions. These results are confirmed by the increase of T-O2 interatomic distance. With respect to crystallisation of cast basalt products, TiO₂ is not suitable as a nucleation admixture because of its "solubility" in clinopyroxenes. |
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