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 160
Belov , N.V. , and Mokeeva , V.I. ( 1954 ) The crystal structure of ilvaite , Trudy . Inst . Kristallogr . Akad . Nauk SSSR 9 , 89-102 ( in Russian ) . Beran , A. , and Bittner , H. ( 1974 ) Untersuchungen zur Kristallchemie des Ilvaits ...
Belov , N.V. , and Mokeeva , V.I. ( 1954 ) The crystal structure of ilvaite , Trudy . Inst . Kristallogr . Akad . Nauk SSSR 9 , 89-102 ( in Russian ) . Beran , A. , and Bittner , H. ( 1974 ) Untersuchungen zur Kristallchemie des Ilvaits ...
Page 165
The same cannot yet be claimed for crystal structures . ... Furthermore , the anisotropy of the susceptibility or magnetization measured in different directions on single crystals provides information on the crystal field interaction .
The same cannot yet be claimed for crystal structures . ... Furthermore , the anisotropy of the susceptibility or magnetization measured in different directions on single crystals provides information on the crystal field interaction .
Page 219
tively on lattice imperfections , which were found to vary strongly between different crystals . ... Each crystal was examined before and after the experiment by X - ray diffraction . The crystals were aligned on X - ray oscillation ...
tively on lattice imperfections , which were found to vary strongly between different crystals . ... Each crystal was examined before and after the experiment by X - ray diffraction . The crystals were aligned on X - ray oscillation ...
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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+ 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
Bibliographic information
| Title | Structural and Magnetic Phase Transitions in Minerals Volume 7 of Advances in Physical Geochemistry |
| Editors | S. Ghose, J.M.D. Coey, E. Salje |
| Contributors | S. Ghose, O. Ballet, T. Brückel, J.M.D. Coey, M.S.T. Bukowinski, E. Salje, B.P. Burton, P.M. Davidson, G. Dolino, H. Fuess, W. Lottermoser, M. Matsui, Y. Matsui, B. Palosz, W. Prandl, D.M. Sherman, G.H. Wolf, B. Wruck |
| Edition | illustrated |
| Publisher | Springer New York, 1988 |
| Original from | the University of California |
| Digitized | 11 Apr 2008 |
| ISBN | 0387967109, 9780387967103 |
| Length | 244 pages |
| Subjects | › › Science / Chemistry / Inorganic Science / Chemistry / Physical & Theoretical Science / Earth Sciences / Mineralogy Science / Physics / Condensed Matter Science / Physics / Crystallography |
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