Magma Redox Geochemistry. Группа авторов
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10 Part III: Tools and Techniques to Characterize the Redox and its Effect on Isotope Partitioning 13 How to Measure the Oxidation State of Multivalent Elements in Minerals, Glasses, and Melts? 13.1. INTRODUCTION 13.2. WET‐CHEMICAL ANALYSES 13.3. ELECTRONIC MICROPROBE 13.4. MÖSSBAUER SPECTROSCOPY 13.5. OPTICAL ABSORPTION SPECTROSCOPY 13.6. X‐RAY ABSORPTION SPECTROSCOPY 13.7. RAMAN SPECTROSCOPY 13.8. IN SITU REDOX DETERMINATION AT HIGH TEMPERATURE OR AT HIGH PRESSURE 13.9. CONCLUSION ACKNOWLEDGMENTS REFERENCES 14 Oxidation State, Coordination, and Covalency Controls on Iron Isotopic Fractionation in Earth’s Mantle and Crust 14.1. INTRODUCTION 14.2. THEORY: EQUILIBRIUM ISOTOPIC FRACTIONATION FROM VIBRATIONAL PROPERTIES 14.3. CALCULATION OF VIBRATIONAL PROPERTIES 14.4. IRON ISOTOPE STUDIES BASED ON NRIXS OR DFT 14.5. COMPARISON OF EQUILIBRIUM FRACTIONATION FACTORS DERIVED FROM VARIOUS TECHNIQUES 14.6. PARAMETERS CONTROLLING EQUILIBRIUM FRACTIONATION FACTORS 14.7. SELECTED APPLICATIONS TO THE INTERPRETATION OF IRON ISOTOPIC VARIATIONS IN IGNEOUS ROCKS 14.8. CONCLUSIONS AND PERSPECTIVES ACKNOWLEDGMENTS REFERENCES 15 The Role of Redox Processes in Determining the Iron Isotope Compositions of Minerals, Melts, and Fluids 15.1. INTRODUCTION 15.2. PRINCIPLES AND NOMENCLATURE 15.3. METHODS FOR THE CALIBRATION OF IRON ISOTOPE FRACTIONATION FACTORS 15.4. FUNDAMENTAL CONTROLS ON ISOTOPIC FRACTIONATION BETWEEN MINERALS, MELTS, AND FLUIDS 15.5. EFFECT OF REDOX PROCESSES IN INFLUENCING IRON ISOTOPE FRACTIONATION IN NATURAL SYSTEMS 15.6. CONCLUSION ACKNOWLEDGMENTS