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The rates of Fe–Mg interdiffusion in the Earth’s materials are of fundamental importance to a wide range of geochemistry and geophysics problems. In order that the Earth Scientist may readily… Click to show full abstract
The rates of Fe–Mg interdiffusion in the Earth’s materials are of fundamental importance to a wide range of geochemistry and geophysics problems. In order that the Earth Scientist may readily apply the available experimentally determined diffusion rates to such problems, a brief review of experimental data for Fe–Mg interdiffusion in mantle minerals is presented concerning new advances and some recent applications. Perspectives for the future are also suggested.
Keywords:
overview interdiffusion;
geochemistry;
interdiffusion mantle;
mantle minerals
Journal Title: Surveys in Geophysics
Year Published: 2017
Link to full text (if available)
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Journal Title: Surveys in Geophysics
Year Published: 2017
Link to full text (if available)
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recommendations!