Strong site preference of Co2+ in olivine, Co1.10Mg0.90SiO4
- 1 January 1974
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 47 (2) , 131-140
- https://doi.org/10.1007/bf00372114
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Some Ordering of Iron and Magnesium at the Octahedrally Coordinated Sites in a Magnesium-rich OlivineNature, 1970
- The partitioning of cations between coexisting single- and multi-site phases with application to the assemblages: orthopyroxene-clinopyroxene and orthopyroxene-olivineGeochimica et Cosmochimica Acta, 1969
- X-ray scattering factors computed from numerical Hartree–Fock wave functionsActa Crystallographica Section A, 1968
- Unit cell dimensions of some synthetic olivine group solid solutionsGEOCHEMICAL JOURNAL, 1968
- Hyperfine Splitting of Fe57 and Mg-Fe Order-Disorder in Orthopyroxenes (MgSiO3-FeSiO3 Solid Solution)The Journal of Geology, 1967
- Mg2+– Fe2+order in an orthopyroxene, Mg0.93Fe1.07Si2O6Zeitschrift für Kristallographie, 1965
- Anomalous dispersion corrections computed from self-consistent field relativistic Dirac–Slater wave functionsActa Crystallographica, 1965
- Site of Preference Energy and Selective Uptake of Transition-Metal Ions from a MagmaScience, 1964
- Applications of the crystal-field theory to the inclusion of trace transition elements in minerals during magmatic differentiationGeochimica et Cosmochimica Acta, 1964
- Apparatus for phase-equilibrium measurements at pressures up to 50 kilobars and temperatures up to 1750°CJournal of Geophysical Research, 1960