Structural and Magnetic Phase Transitions in Minerals |
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Page 116
A number of iron ( II ) chelates ( e.g. , the iron phenanthroline complexes ) also contain low - spin Fe2 + ( Drickamer and Frank , 1973 ) or exhibit the HS – LS transition of Fe2 + with moderate pressures . In all of these complexes ...
A number of iron ( II ) chelates ( e.g. , the iron phenanthroline complexes ) also contain low - spin Fe2 + ( Drickamer and Frank , 1973 ) or exhibit the HS – LS transition of Fe2 + with moderate pressures . In all of these complexes ...
Page 162
Iron is by far the most abundant transition element in the earth ; in fact , it is 40 times as abundant in the crust as all other magnetic elements put together , so the emphasis here falls naturally on iron silicates , although ...
Iron is by far the most abundant transition element in the earth ; in fact , it is 40 times as abundant in the crust as all other magnetic elements put together , so the emphasis here falls naturally on iron silicates , although ...
Page 183
Coey , J.M.D. ( 1987b ) Magnetic properties of iron in soil oxides and clay minerals . In Iron in Soils and Sediments , edited by J.A. Stucki and B.A. Goodman . Riedel , Dordrecht . Ch . 14 . Coey , J.M.D. , and Ballet , O. ( 1978 ) La ...
Coey , J.M.D. ( 1987b ) Magnetic properties of iron in soil oxides and clay minerals . In Iron in Soils and Sediments , edited by J.A. Stucki and B.A. Goodman . Riedel , Dordrecht . Ch . 14 . Coey , J.M.D. , and Ballet , O. ( 1978 ) La ...
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Contents
Incommensurate Phase Transitions in Quartz and Berlinite | 17 |
Phase Separation in Quadrilateral Pyroxenes and Olivines | 39 |
Multicritical Phase Relations in Minerals | 60 |
Copyright | |
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Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Limited preview - 2012 |
Common terms and phrases
antiferromagnetic appears applied approximation atoms axis Ballet behavior bond calculated cation Chem chemical cluster Coey components composition constant corresponding coupling critical crystal decreases density dependence described determined diffraction direction disordered Dolino effect electron energy equilibrium estimated et al exchange experimental experiments Fe2+ ferromagnetic field function Ghose give given heat ilvaite inc phase increases indicate interactions ions iron lattice layers Lindsley lower mantle magnetic magnetic order materials measurements Mineral mode Mössbauer natural neutron observed obtained occur octahedral olivines order parameter pairs perovskite phase diagrams phase transition Phys physical pigeonite polytypes positions possible potential predicted pressure properties pyroxenes quartz range respectively Salje sample shown shows silicates solid solution space group spin stability structure symmetry Table temperature theory thermodynamic tion transformation unit variation