2002
DOI: 10.1023/a:1021228119983
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Cited by 8 publications
(3 citation statements)
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“…XRD of the initial olivine (Figure ) shows the same main lines as those in the theoretical diffractogram of (Mg 0.9 Fe 0.1 ) 2 SiO 4 , which are close to those of the Mg 2 SiO 4 forsterite visualized by its 100-intensity line at 28.2° 2θ, and a spinel cubic phase, which could be either γ-Fe 2 O 3 , Fe 3 O 4 , or MgFe 2 O 4 magnesioferrite (and/or members of solid solutions such as MgFe 2 O 4 −Fe 3 O 4 and MgFe 2 O 4 −γ-Fe 2 O 3 ) . XRD does not permit us to distinguish between those three phases, which have nearly the same diffraction patterns .…”
Section: Resultssupporting
confidence: 63%
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“…XRD of the initial olivine (Figure ) shows the same main lines as those in the theoretical diffractogram of (Mg 0.9 Fe 0.1 ) 2 SiO 4 , which are close to those of the Mg 2 SiO 4 forsterite visualized by its 100-intensity line at 28.2° 2θ, and a spinel cubic phase, which could be either γ-Fe 2 O 3 , Fe 3 O 4 , or MgFe 2 O 4 magnesioferrite (and/or members of solid solutions such as MgFe 2 O 4 −Fe 3 O 4 and MgFe 2 O 4 −γ-Fe 2 O 3 ) . XRD does not permit us to distinguish between those three phases, which have nearly the same diffraction patterns .…”
Section: Resultssupporting
confidence: 63%
“…This apparent ferrous doublet is in fact a superposition of two doublets caused by Fe 2+ at the M1 and M2 sites of the olivine lattice. These doublets strongly overlap and are therefore not resolvable; they had to be fitted by one hyperfine pattern …”
Section: Resultsmentioning
confidence: 99%
“…The parameters of the three subspectra for Ni/olivine calcined at 1100 and 1400 °C are given in Table . The quadrupole doublet present in the Mössbauer spectra with an isomer shift of ∼1.12 mm s -1 and quadrupole splitting of ∼3.06 mm s -1 is due to Fe 2+ ions in the olivine structure , They can be attributed to the iron in the form of α-Fe 2 O 3 and spinel phase (MgFe 2 O 4 ).…”
Section: Resultsmentioning
confidence: 98%