F. Scordari
University of Bari
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Mineralogy and Petrology | 1981
F. Scordari
The mineral fibroferrite has the chemical formula Fe(OH)SO4·xH2O; the value forx has not been definitely settled, but as a rule it is found to be near five. Several symmetries are given in the literature.
Mineralogy and Petrology | 1976
G. Giacovazzo; F. Scordari; A. Todisco; Silvio Menchetti
The crystal structure of metavoltine from Sierra Gorda, Chile, has been solved from photographic X-ray data by the heavy atom method. The space group used wasP3 witha=9.575(5) andc=18.17(1)A; cell content: K2Na6 (Fe2+, Cu, Zn)Fe 6 3+ (SO4)12O2·18H2O. From the relatively small number and the somewhat poor quality of the X-ray data, the least squares refinement did not give very satisfactory results-especially so for the light atoms. Therefore, steric considerations and information from the Fourier maps were also used when choosing the final atomic coordinates. The salient features of the structure are clusters of Fe 3 3+ O(H2O)3(SO4)6 with Fe3+ in octahedral coordination, and Fe2+(H2O)6 octahedra. The Na+ ions show octahedral coordination, the K+ ions irregular nine coordination.
Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry | 1973
C. Giacovazzo; Silvio Menchetti; F. Scordari
Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry | 1975
C. Giacovazzo; F. Scordari; Silvio Menchetti
Mineralogy and Petrology | 1975
F. Scordari; F. Vurro; Silvio Menchetti
Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry | 1973
C. Giacovazzo; Silvio Menchetti; F. Scordari
Mineralogy and Petrology | 1981
F. Scordari
Naturwissenschaften | 1970
C. Giacovazzo; Silvio Menchetti; F. Scordari
Mineralogy and Petrology | 1981
F. Scordari
Mineralogy and Petrology | 1976
G. Giacovazzo; F. Scordari; A. Todisco; Silvio Menchetti