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An Overview of Fe-Mg Interdiffusion in Mantle Minerals
Baohua Zhang
2017
发表期刊Surveys in Geophysics
卷号38期号:4页码:727–755
摘要

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.

关键词High Temperature And High Pressure mantle Mineral fe–mg Interdiffusion point Defects
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/42920512-1/8083
专题地球内部物质高温高压实验室
作者单位Key Laboratory for High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
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Baohua Zhang. An Overview of Fe-Mg Interdiffusion in Mantle Minerals[J]. Surveys in Geophysics,2017,38(4):727–755.
APA Baohua Zhang.(2017).An Overview of Fe-Mg Interdiffusion in Mantle Minerals.Surveys in Geophysics,38(4),727–755.
MLA Baohua Zhang."An Overview of Fe-Mg Interdiffusion in Mantle Minerals".Surveys in Geophysics 38.4(2017):727–755.
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