Structural and Magnetic Phase Transitions in MineralsThis volume in Advances in Physical Geochemistry presents the latest synthesis of theory and experimental data pertaining to structural and magnetic phase transitions in a variety of geochemically important minerals. The book is the first to cover the impact of this rapidly progressing area of solid state physics in earth sciences and reflects its growing significance for mineralogy and petrology. |
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Page 40
Perhaps the most widely used model is that of Wood and Banno ( 1973 ) , in which a prescription for projecting natural compositions back to the diopside - enstatite ( Di - En ) join permits evaluation of the temperature of the reaction ...
Perhaps the most widely used model is that of Wood and Banno ( 1973 ) , in which a prescription for projecting natural compositions back to the diopside - enstatite ( Di - En ) join permits evaluation of the temperature of the reaction ...
Page 41
Perhaps the most widely used model is that of Wood and Banno ( 1973 ) , in which a prescription for projecting natural compositions back to the diopside - enstatite ( Di - En ) join permits evaluation of the temperature of the reaction ...
Perhaps the most widely used model is that of Wood and Banno ( 1973 ) , in which a prescription for projecting natural compositions back to the diopside - enstatite ( Di - En ) join permits evaluation of the temperature of the reaction ...
Page 148
Natural Orthorhombic Ilvaites Why certain natural ilvaites are orthorhombic under ambient conditions is not clear , because no simple correlation of impurity content with the monoclinic versus orthorhombic symmetry exists ...
Natural Orthorhombic Ilvaites Why certain natural ilvaites are orthorhombic under ambient conditions is not clear , because no simple correlation of impurity content with the monoclinic versus orthorhombic symmetry exists ...
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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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Other editions - View all
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+ Fe3+ 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