An EPR study of Mn2+ and Fe3+ in dolomites
- 1 January 1986
- journal article
- Published by Springer Nature in Physics and Chemistry of Minerals
- Vol. 13 (5) , 331-336
- https://doi.org/10.1007/bf00308350
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Correlation of Zero-Field Splittings and Site Distortions. IX. Fe3+ and Cr3+ in β -Ga2O3Zeitschrift für Naturforschung A, 1987
- Crystal structure refinements of magnesite, calcite, rhodochrosite, siderite, smithonite, and dolomite, with discussion of some aspects of the stereochemistry of calcite type carbonatesZeitschrift für Kristallographie - Crystalline Materials, 1981
- Correlation of zero-field splittings and site distortions: Variation of
b 2 FOR Mn2+ with ligand and coordination numberChemical Physics Letters, 1981 - Variation of hyperfine splitting constants for 3d5-ions with interatomic distanceJournal of Physics and Chemistry of Solids, 1980
- Refinement and comparison of the crystal structures of a dolomite and of an Fe-rich ankeriteTschermaks Mineralogische und Petrographische Mitteilungen, 1977
- EPR study of Mn2+in diopsideJournal of Physics C: Solid State Physics, 1975
- Electron Paramagnetic Resonance Study of Ordered Mn2+ in Mg2SiO4The Journal of Chemical Physics, 1970
- The Allowed and Forbidden Transitions in the Paramagnetic Resonance of the Manganese Ion in Trigonal Sites in Apatite and SmithsoniteAustralian Journal of Physics, 1964
- Subsolidus Relations in the System CaCO3-MgCO3-MnCO3The Journal of Geology, 1960
- Paramagnetic Resonance Absorption ofin Single Crystals of CaCPhysical Review B, 1954