Wx. Xu et al., MODIFIED LATTICE-PARAMETER CURIE-TEMPERATURE DIAGRAMS FOR TITANOMAGNETITE TITANOMAGHEMITE WITHIN THE QUADRILATERAL FE3O4-FE2TIO4-FE2O3-FE2TIO5/, Geophysical research letters, 23(20), 1996, pp. 2811-2814
Magnetic and mineralogical data were obtained on a sequence of titanom
agnetite - titanomaghemite solid solutions from four basalt samples (0
to 70 Ma) dredged from four sites along a traverse normal to the mid-
Atlantic Ridge. Data which characterized magnetic iron oxides with the
spinel structure include Mossbauer, XRD (including Rietveld structure
refinement), TEM/AEM, and magnetic data. The data indicate a sequence
ranging from nearly unoxidized titanomagnetite to near end-member tit
anomaghemite. Compositions of samples with intermediate values of oxid
ation parameter, Z, varied significantly from those estimated using pr
eviously determined relations between lattice parameters and compositi
ons. The data of this study, in conjunction with those of selected ref
erences, lead to more accurate contoured diagrams for Curie temperatur
e and lattice parameter (as consistent with Vegard's law) for the quad
rilateral Fe3O4-Fe2TiO4-Fe2O3-Fe2TiO5.