Abstract
The compound Ca4Fe1.5Al17.67O32 was synthesized at 2.5 GPa and 1250 °C using a piston-cylinder apparatus. The crystal structure, determined from single-crystal X-ray diffraction data collected at 295 K (tetragonal, space group I4̄ - 2d, a = 20.1847(14) Å, c = 5.6203(6) Å, V = 2289.83(3) Å3, Z = 4) was refined to a final R-index of 0.024 for 1229 independent observed reflections and 130 parameters. The main building units comprising the compound are 11.8 × 7.2 Å wide spinel-type ribbons running parallel to [001], which are connected via corner-sharing (Fe,Al)O6-octahedra. Additional linkage between the spinel units is provided by AlO4-tetrahedra residing on the 4̄-axis as well as by Ca cations, in sevenfold coordination with oxygen attached to the spinel-like building units. Refinement of site occupancies reveals that the incorporation of Fe occurs at two of four octahedral and at two of three tetrahedral sites. Apparently, Ca4Fe1.5Al17.67O32 represents a new structure type exhibiting more pronounced structural modifications relative to the spinel aristotype compared with the socalled spinelloid structures. Furthermore, this synthetic compound contains Fe2+ in tetrahedral coordination, which is relatively uncommon among inorganic materials.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- First-principles modeling of the infrared spectrum of kaolinite
- Determination of the limiting fictive temperature of silicate glasses from calorimetric and dilatometric methods: Application to low-temperature liquid volume measurements
- Enthalpies of formation of tremolite and talc by high-temperature solution calorimetry – a consistent picture
- Evidence for an I2/a to Imab phase transition in the silica polymorph moganite at ~570 K
- Thermal decomposition of rhombohedral KClO3 from 29–76 kilobars and implications for the molar volume of fluid oxygen at high pressures
- High-pressure behavior of clinochlore
- Structure and elasticity of wadsleyite at high pressures
- Determination of the fluid–absent solidus and supersolidus phase relationships of MORB-derived amphibolites in the range 4–14 kbar
- F-rich phlogopite stability in ultra-high-temperature metapelites from the Napier Complex, East Antarctica
- Instability of Al2SiO5 “triple-point” assemblages in muscovite+biotite+quartz-bearing metapelites, with implications
- Stability of osumilite coexisting with spinel solid solution in metapelitic granulites at high oxygen fugacity
- Geikielite exsolution in spinel
- Aeromagnetic anomalies, magnetic petrology, and rock magnetism of hemo-ilmenite- and magnetite-rich cumulate rocks from the Sokndal Region, South Rogaland, Norway
- Minor element chemistry of hemo-ilmenite and magnetite in cumulate rocks from the Sokndal Region, South Rogaland, Norway
- Crystal structure analysis of synthetic Ca4Fe1.5Al17.67O32: A high-pressure, spinel-related phase
- Crystal structure of phase X, a high pressure alkali-rich hydrous silicate and its anhydrous equivalent
- Fluoro-edenite from Biancavilla (Catania, Sicily, Italy): Crystal chemistry of a new amphibole end-member
- Description and crystal structure of turtmannite, a new mineral with a 68 Å period related to mcgovernite
- The crystal structure of low melanophlogite
- Crystal structures of Na and K aluminate mullites
- From mastodon ivory to gemstone: The origin of turquoise color in odontolite
- Letters. Elasticity of single-crystal calcite and rhodochrosite by Brillouin spectroscopy
- Ikaite, CaCO3·6H2O: Cold comfort for glendonites as paleothermometers