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.
Publication name | SURVEYS IN GEOPHYSICS, 38 (4):727-755; 10.1007/s10712-017-9415-5 JUL 2017 |
Author(s) | Zhang, Baohua |
Corresponding author(s) | ZHANG Baohua zhangbaohua@vip.gyig.ac.cn Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths In, Guiyang 550081, Peoples R China. |
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